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  • 1
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    A new modern analogue reference dataset and its application to the 430-kyr pollen record from Lake Biwa
    PANGAEA
    In:  Supplement to: Tarasov, Pavel E; Nakagawa, Takeshi; Demske, Dieter; Österle, Hermann; Igarashi, Yaeko; Kitagawa, Junko; Mokhova, Lyudmila M; Bazarova, Valentina B; Okuda, Masaaki; Gotanda, Katsuya; Miyoshi, Norio; Fujiki, Toshiyuki; Takemura, Keiji; Yonenobu, Hitoshi; Fleck, Andreas (2011): Progress in the reconstruction of Quaternary climate dynamics in the Northwest Pacific: A new modern analogue reference dataset and its application to the 430-kyr pollen record from Lake Biwa. Earth-Science Reviews, 108(1-2), 64-79, https://doi.org/10.1016/j.earscirev.2011.06.002
    Details
    Publication Date: 2023-05-12
    Description: This study presents a newly compiled dataset of modern pollen and climate data from 798 sites across Japan and the Russian Far East. This comprehensive reference dataset combined with the modern analogue technique (MAT) provides a powerful tool for pollen-based reconstruction of the Quaternary Northwest Pacific climate. Pollen-derived reconstruction of the modern climate at the reference pollen-sampling sites matches well with the estimated modern climate values (R2 values vary between 0.79 and 0.95, and RMSEP values vary between 5.8 and 9.7% of the modern climatic range for all nine tested variables). The successful testing of the method encourages its application to the fossil pollen records. We used a coarse-resolution pollen record from Lake Biwa to reconstruct glacial-interglacial climate dynamics in central Japan since ~438 kyr and compared it to the earlier reconstruction based on a less representative reference dataset. The current and earlier results consistently demonstrate that the coldest glacial intervals experienced pronounced cooling in winter and moderate cooling in summer, supporting the growth of cool mixed forest (COMX) where warm mixed forest (WAMX) predominates today. During the last glacial, maximum (~24 kyr BP) mean temperatures of the coldest (MTCO) and warmest (MTWA) month were about -13 °C (RMSEP = 2.34 °C) and 21 °C (RMSEP = 1.66 °C) respectively, and annual precipitation (PANN) was about 800 mm (RMSEP = 158.06 mm). During the thermal optimums of the interglacial intervals, the temperatures of the coldest and warmest month were above 0 °C and 25 °C respectively, leading to the reconstruction of WAMX and temperate conifer forest (TECO). Although both these vegetation types grow in the southern part of Japan today, WAMX requires warmer space. The presence of WAMX during marine isotope stages (MIS) 11 and 1, and its absence during MIS 9 and MIS 5 contradict the marine isotope and Antarctic ice records, suggesting that the latter two interglacials were the warmest of the last 800 kyr. The apparent contradiction allows at least three different explanations including low temporal resolution of the pollen record; different trends in CO2 concentrations during 'short' and 'long' interglacials; and regional climate variability and non-linear response of different regions to the global forcing. More definitive conclusions will be possible on the basis of forthcoming high-resolution pollen records from central Japan.
    Type: Dataset
    Format: application/zip, 4 datasets
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 2
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    (Table S4) Reconstructed climate variables derived from the Lake Biwa pollen record
    PANGAEA
    Details
    Publication Date: 2023-05-12
    Keywords: AGE; DRILL; Drilling/drill rig; Japan; Lake_Biwa; Modern analog technique (MAT); Number of analogues; Precipitation, annual mean; Precipitation, annual mean, maximum; Precipitation, annual mean, minimum; Precipitation, Apr-Sep; Precipitation, Apr-Sep, maximum; Precipitation, Apr-Sep, minimum; Precipitation, Oct-Mar; Precipitation, Oct-Mar, maximum; Precipitation, Oct-Mar, minimum; Temperature, annual mean; Temperature, annual mean, maximum; Temperature, annual mean, minimum; Temperature, coldest month; Temperature, coldest month, maximum; Temperature, coldest month, minimum; Temperature, difference; Temperature, difference, maximum; Temperature, difference, minimum; Temperature, warmest month; Temperature, warmest month, maximum; Temperature, warmest month, minimum; Temperature coldness index; Temperature coldness index, maximum; Temperature coldness index, minimum; Temperature warmth index; Temperature warmth index, maximum; Temperature warmth index, minium
    Type: Dataset
    Format: text/tab-separated-values, 3780 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 3
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    (Table S1) Modern climate variables of 798 modern surface pollen sampling sites
    PANGAEA
    Details
    Publication Date: 2023-05-12
    Keywords: AMUR1; AMUR10; AMUR11; AMUR12; AMUR13; AMUR14; AMUR15; AMUR16; AMUR17; AMUR18; AMUR19; AMUR2; AMUR20; AMUR21; AMUR22; AMUR23; AMUR24; AMUR25; AMUR26; AMUR27; AMUR28; AMUR29; AMUR3; AMUR31; AMUR32; AMUR33; AMUR34; AMUR35; AMUR36; AMUR37; AMUR38; AMUR39; AMUR4; AMUR40; AMUR43; AMUR44; AMUR45; AMUR46; AMUR47; AMUR48; AMUR49; AMUR5; AMUR50; AMUR51; AMUR52; AMUR53; AMUR54; AMUR55; AMUR56; AMUR57; AMUR6; AMUR7; AMUR8; AMUR9; China; DEPTH, sediment/rock; Elevation of event; Estimated by Polygon 2.3.3; Event label; Hand corer; HCOR; HOKK_02; HOKK_05; HOKK_07; HOKK_08; HOKK_10; HOKK_11; HOKK_14; Japan; Jss-001; Jss-002; Jss-003; Jss-004; Jss-005; Jss-006; Jss-007; Jss-008; Jss-009; Jss-010; Jss-011; Jss-012; Jss-013; Jss-014; Jss-015; Jss-016; Jss-017; Jss-018; Jss-019; Jss-020; Jss-021; Jss-022; Jss-023; Jss-024; Jss-025; Jss-026; Jss-027; Jss-028; Jss-029; Jss-030; Jss-031; Jss-032; Jss-033; Jss-034; Jss-035; Jss-036; Jss-037; Jss-038; Jss-039; Jss-040; Jss-041; Jss-042; Jss-043; Jss-044; Jss-045; Jss-046; Jss-047; Jss-048; Jss-049; Jss-050; Jss-051; Jss-052; Jss-053; Jss-054; Jss-055; Jss-056; Jss-057; Jss-058; Jss-059; Jss-060; Jss-061; Jss-062; Jss-063; Jss-064; Jss-065; Jss-066; Jss-067; Jss-068; Jss-069; Jss-070; Jss-071; Jss-072; Jss-073; Jss-074; Jss-075; Jss-076; Jss-077; Jss-078; Jss-079; Jss-080; Jss-081; Jss-082; Jss-083; Jss-084; Jss-085; Jss-086; Jss-087; Jss-088; Jss-089; Jss-090; Jss-091; Jss-092; Jss-093; Jss-094; Jss-095; Jss-096; Jss-097; Jss-098; Jss-099; Jss-100; Jss-101; Jss-102; Jss-103; Jss-104; Jss-105; Jss-106; Jss-107; Jss-108; Jss-109; Jss-110; Jss-111; Jss-112; Jss-113; Jss-114; Jss-115; Jss-116; Jss-117; Jss-118; Jss-119; Jss-120; Jss-121; Jss-122; Jss-123; Jss-124; Jss-125; Jss-126; Jss-127; Jss-128; Jss-129; Jss-130; Jss-131; Jss-132; Jss-133; Jss-134; Jss-135; Jss-136; Jss-137; Jss-138; Jss-139; Jss-140; Jss-141; Jss-142; Jss-143; Jss-144; Jss-145; Jss-146; Jss-147; Jss-148; Jss-149; Jss-150; Jss-151; Jss-152; Jss-153; Jss-154; Jss-155; Jss-156; Jss-157; Jss-158; Jss-159; Jss-160; Jss-161; Jss-162; Jss-163; Jss-164; Jss-165; Jss-166; Jss-167; Jss-168; Jss-169; Jss-170; Jss-171; Jss-172; Jss-173; Jss-174; Jss-175; Jss-176; Jss-177; Jss-178; Jss-179; Jss-180; Jss-181; Jss-182; Jss-183; Jss-184; Jss-185; Jss-186; Jss-187; Jss-188; Jss-189; Jss-190; Jss-191; Jss-192; Jss-193; Jss-194; Jss-195; Jss-196; Jss-197; Jss-198; Jss-199; Jss-200; Jss-201; Jss-202; Jss-203; Jss-204; Jss-205; Jss-206; Jss-207; Jss-208; Jss-209; Jss-210; Jss-211; Jss-212; Jss-213; Jss-214; Jss-215; Jss-216; Jss-217; Jss-218; Jss-219; Jss-220; Jss-221; Jss-222; Jss-223; Jss-224; Jss-225; Jss-226; Jss-227; Jss-228; Jss-229; Jss-230; Jss-231; Jss-232; Jss-233; Jss-234; Jss-235; Jss-236; Jss-237; Jss-238; Jss-239; Jss-240; Jss-241; Jss-242; Jss-243; Jss-244; Jss-245; Jss-246; Jss-247; Jss-248; Jss-249; Jss-250; Jss-251; Jss-252; Jss-253; Jss-254; Jss-255; Jss-256; Jss-257; Jss-258; Jss-259; Jss-260; Jss-261; Jss-262; Jss-263; Jss-264; Jss-265; Jss-266; Jss-267; Jss-268; Jss-269; Jss-270; Jss-271; Jss-272; Jss-273; Jss-274; Jss-275; Jss-276; Jss-277; Jss-278; Jss-279; Jss-280; Jss-281; Jss-282; Jss-283; Jss-284; Jss-285; Jun-286; Jun-287; Jun-288; Jun-289; Jun-290; Jun-291; Jun-292; Jun-293; Jun-294; Jun-295; Jun-296; Jun-297; Jun-298; Jun-299; Jun-300; Jun-301; Jun-302; Jun-303; Jun-304; Jun-305; Jun-306; Jun-307; Jun-308; Jun-310; Jun-311; Jun-312; Jun-313; Jun-314; Jun-315; Jun-316; Jun-317; Jun-318; Jun-319; Jun-320; Jun-321; Jun-322; Jun-323; Jun-324; Jun-325; Jun-326; Jun-327; Jun-328; KUNASH1; KUNASH2; KUNASH3; KUNASH4; KUNASH5; KUNASH6; KUNASH7; KUNASH8; Latitude of event; Longitude of event; MOKH1; MOKH10; MOKH100; MOKH101; MOKH102; MOKH103; MOKH104; MOKH105; MOKH106; MOKH107; MOKH108; MOKH109; MOKH11; MOKH110; MOKH111; MOKH112; MOKH113; MOKH114; MOKH115; MOKH116; MOKH117; MOKH118; MOKH119; MOKH12; MOKH120; MOKH121; MOKH122; MOKH123; MOKH124; MOKH125; MOKH126; MOKH127; MOKH128; MOKH129; MOKH13; MOKH130; MOKH131; MOKH133; MOKH134; MOKH135; MOKH136; MOKH137; MOKH138; MOKH139; MOKH14; MOKH140; MOKH141; MOKH142; MOKH143; MOKH144; MOKH145; MOKH146; MOKH147; MOKH148; MOKH149; MOKH15; MOKH150; MOKH151; MOKH152; MOKH153; MOKH154; MOKH155; MOKH156; MOKH157; MOKH158; MOKH159; MOKH16; MOKH160; MOKH161; MOKH162; MOKH163; MOKH164; MOKH165; MOKH166; MOKH167; MOKH168; MOKH169; MOKH17; MOKH170; MOKH171; MOKH172; MOKH173; MOKH174; MOKH175; MOKH176; MOKH177; MOKH178; MOKH18; MOKH180; MOKH181; MOKH182; MOKH183; MOKH184; MOKH185; MOKH186; MOKH187; MOKH188; MOKH189; MOKH19; MOKH194; MOKH195; MOKH196; MOKH197; MOKH199; MOKH2; MOKH200; MOKH202; MOKH204; MOKH206; MOKH207; MOKH208; MOKH209; MOKH21; MOKH210; MOKH211; MOKH212; MOKH213; MOKH214; MOKH215; MOKH216; MOKH217; MOKH218; MOKH219; MOKH22; MOKH220; MOKH221; MOKH223; MOKH224; MOKH225; MOKH226; MOKH227; MOKH228; MOKH23; MOKH231; MOKH233; MOKH234; MOKH237; MOKH238; MOKH239; MOKH24; MOKH240; MOKH241; MOKH242; MOKH25; MOKH26; MOKH27; MOKH28; MOKH29; MOKH3; MOKH30; MOKH31; MOKH32; MOKH33; MOKH34; MOKH35; MOKH36; MOKH38; MOKH39; MOKH40; MOKH41; MOKH42; MOKH43; MOKH44; MOKH45; MOKH46; MOKH47; MOKH48; MOKH49; MOKH50; MOKH51; MOKH53; MOKH54; MOKH55; MOKH56; MOKH59; MOKH6; MOKH60; MOKH61; MOKH62; MOKH63; MOKH64; MOKH65; MOKH66; MOKH67; MOKH68; MOKH69; MOKH7; MOKH71; MOKH72; MOKH73; MOKH75; MOKH76; MOKH77; MOKH78; MOKH79; MOKH8; MOKH80; MOKH81; MOKH82; MOKH83; MOKH84; MOKH85; MOKH86; MOKH87; MOKH88; MOKH89; MOKH9; MOKH91; MOKH92; MOKH93; MOKH94; MOKH95; MOKH96; MOKH97; MOKH98; MOKH99; Oku-013; Oku-014; Oku-015; Oku-016; Oku-017; Oku-018; Oku-019; Oku-020; Oku-021; Oku-022; Oku-023; Oku-024; Oku-025; Oku-026; Oku-027; Oku-028; Oku-029; Oku-030; Oku-031; Oku-035; Oku-036; Oku-037; Oku-038; Oku-039; Oku-040; Oku-041; Oku-042; Oku-043; Oku-044; Oku-045; Oku-046; Oku-047; Oku-048; Oku-051; Oku-052; Oku-053; Oku-054; Oku-055; Oku-056; Oku-057; Oku-058; Oku-059; Oku-060; Oku-061; Oku-062; Oku-063; Oku-064; Oku-065; Oku-066; Oku-067; Oku-068; Oku-069; Oku-070; Oku-071; Oku-072; Oku-073; Oku-074; Oku-075; Oku-076; Oku-077; Oku-078; Oku-079; Oku-080; Oku-081; Oku-082; Oku-083; Oku-084; Oku-085; Oku-086; Oku-087; Oku-088; Oku-089; Oku-090; Oku-091; Oku-092; Oku-093; Oku-094; Oku-095; Oku-096; Oku-097; Oku-098; Oku-099; Oku-100; Oku-101; Oku-102; Oku-103; Oku-105; Oku-106; Oku-107; Oku-108; Oku-109; Oku-110; Oku-111; Oku-112; Pav_1; Pav_10; Pav_11; Pav_12; Pav_13a; Pav_13b; Pav_14; Pav_15; Pav_16; Pav_17; Pav_18; Pav_19; Pav_2; Pav_20; Pav_21; Pav_22; Pav_23; Pav_24; Pav_25; Pav_3a; Pav_3b; Pav_3c; Pav_3d; Pav_4a; Pav_4b; Pav_4c; Pav_5; Pav_6; Pav_7; Pav_8; Pav_9; Pav_H12-1; Pav_H13-1; Pav_H13-2; Pav_H13-2(2); Pav_H13-3; Pav_H14-1; Pav_H14-2; Pav_H17-1; Pav_H17-2; Pav_H19-1; Pav_H19-2; Pav_H19-3; Pav_H19-4; Pav_H19-4bis; Pav_H19-5; Pav_H19-6; Pav_H20-1; Pav_H20-2; Pav_H20-3; Pav_H20-4; Pav_H20-5; Pav_H20-6; Precipitation, annual mean; Precipitation, Apr-Sep; Precipitation, Oct-Mar; Russia; SAKH_01; SAKH_03; SAKH_04; SAKH_06; SAKH_08; SAKH_10; SAKH_11; SAKH_13; SAKH_15; SAKH_17; SAKH_19; SAKH_21; SAKH_23; SAKH_25; SAKH_26; SAKH_28; SAKH_29; SAKH_31; SAKH_33; SAKH_35; SAKH_36; SAKH_37; SAKH_39; SAKH_40; SAKH_41; SAKH_43; SAKH_45; SAKH_47; SAKH_49; SAKH_51; SAKH_53; SAKH_54; SAKH_55; SAKH_57; SAKH_58; SAKH_59; SAKH_61; SAKH_62; SAKH_63; Temperature, annual mean; Temperature, coldest month; Temperature, difference; Temperature, warmest month; Temperature coldness index; Temperature gradient; Temperature warmth index
    Type: Dataset
    Format: text/tab-separated-values, 7980 data points
    Location Call Number Expected Availability
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  • 4
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    (Table S3) Modern climate variables at the modern surface pollen sites reconstructed using modern-analogue technique and reference pollen-climate dataset
    PANGAEA
    Details
    Publication Date: 2023-05-12
    Keywords: AMUR1; AMUR10; AMUR11; AMUR12; AMUR13; AMUR14; AMUR15; AMUR16; AMUR17; AMUR18; AMUR19; AMUR2; AMUR20; AMUR21; AMUR22; AMUR23; AMUR24; AMUR25; AMUR26; AMUR27; AMUR28; AMUR29; AMUR3; AMUR31; AMUR32; AMUR33; AMUR34; AMUR35; AMUR36; AMUR37; AMUR38; AMUR39; AMUR4; AMUR40; AMUR43; AMUR44; AMUR45; AMUR46; AMUR47; AMUR48; AMUR49; AMUR5; AMUR50; AMUR51; AMUR52; AMUR53; AMUR54; AMUR55; AMUR56; AMUR57; AMUR6; AMUR7; AMUR8; AMUR9; China; DEPTH, sediment/rock; Event label; Hand corer; HCOR; HOKK_02; HOKK_05; HOKK_07; HOKK_08; HOKK_10; HOKK_11; HOKK_14; Japan; Jss-001; Jss-002; Jss-003; Jss-004; Jss-005; Jss-006; Jss-007; Jss-008; Jss-009; Jss-010; Jss-011; Jss-012; Jss-013; Jss-014; Jss-015; Jss-016; Jss-017; Jss-018; Jss-019; Jss-020; Jss-021; Jss-022; Jss-023; Jss-024; Jss-025; Jss-026; Jss-027; Jss-028; Jss-029; Jss-030; Jss-031; Jss-032; Jss-033; Jss-034; Jss-035; Jss-036; Jss-037; Jss-038; Jss-039; Jss-040; Jss-041; Jss-042; Jss-043; Jss-044; Jss-045; Jss-046; Jss-047; Jss-048; Jss-049; Jss-050; Jss-051; Jss-052; Jss-053; Jss-054; Jss-055; Jss-056; Jss-057; Jss-058; Jss-059; Jss-060; Jss-061; Jss-062; Jss-063; Jss-064; Jss-065; Jss-066; Jss-067; Jss-068; Jss-069; Jss-070; Jss-071; Jss-072; Jss-073; Jss-074; Jss-075; Jss-076; Jss-077; Jss-078; Jss-079; Jss-080; Jss-081; Jss-082; Jss-083; Jss-084; Jss-085; Jss-086; Jss-087; Jss-088; Jss-089; Jss-090; Jss-091; Jss-092; Jss-093; Jss-094; Jss-095; Jss-096; Jss-097; Jss-098; Jss-099; Jss-100; Jss-101; Jss-102; Jss-103; Jss-104; Jss-105; Jss-106; Jss-107; Jss-108; Jss-109; Jss-110; Jss-111; Jss-112; Jss-113; Jss-114; Jss-115; Jss-116; Jss-117; Jss-118; Jss-119; Jss-120; Jss-121; Jss-122; Jss-123; Jss-124; Jss-125; Jss-126; Jss-127; Jss-128; Jss-129; Jss-130; Jss-131; Jss-132; Jss-133; Jss-134; Jss-135; Jss-136; Jss-137; Jss-138; Jss-139; Jss-140; Jss-141; Jss-142; Jss-143; Jss-144; Jss-145; Jss-146; Jss-147; Jss-148; Jss-149; Jss-150; Jss-151; Jss-152; Jss-153; Jss-154; Jss-155; Jss-156; Jss-157; Jss-158; Jss-159; Jss-160; Jss-161; Jss-162; Jss-163; Jss-164; Jss-165; Jss-166; Jss-167; Jss-168; Jss-169; Jss-170; Jss-171; Jss-172; Jss-173; Jss-174; Jss-175; Jss-176; Jss-177; Jss-178; Jss-179; Jss-180; Jss-181; Jss-182; Jss-183; Jss-184; Jss-185; Jss-186; Jss-187; Jss-188; Jss-189; Jss-190; Jss-191; Jss-192; Jss-193; Jss-194; Jss-195; Jss-196; Jss-197; Jss-198; Jss-199; Jss-200; Jss-201; Jss-202; Jss-203; Jss-204; Jss-205; Jss-206; Jss-207; Jss-208; Jss-209; Jss-210; Jss-211; Jss-212; Jss-213; Jss-214; Jss-215; Jss-216; Jss-217; Jss-218; Jss-219; Jss-220; Jss-221; Jss-222; Jss-223; Jss-224; Jss-225; Jss-226; Jss-227; Jss-228; Jss-229; Jss-230; Jss-231; Jss-232; Jss-233; Jss-234; Jss-235; Jss-236; Jss-237; Jss-238; Jss-239; Jss-240; Jss-241; Jss-242; Jss-243; Jss-244; Jss-245; Jss-246; Jss-247; Jss-248; Jss-249; Jss-250; Jss-251; Jss-252; Jss-253; Jss-254; Jss-255; Jss-256; Jss-257; Jss-258; Jss-259; Jss-260; Jss-261; Jss-262; Jss-263; Jss-264; Jss-265; Jss-266; Jss-267; Jss-268; Jss-269; Jss-270; Jss-271; Jss-272; Jss-273; Jss-274; Jss-275; Jss-276; Jss-277; Jss-278; Jss-279; Jss-280; Jss-281; Jss-282; Jss-283; Jss-284; Jss-285; Jun-286; Jun-287; Jun-288; Jun-289; Jun-290; Jun-291; Jun-292; Jun-293; Jun-294; Jun-295; Jun-296; Jun-297; Jun-298; Jun-299; Jun-300; Jun-301; Jun-302; Jun-303; Jun-304; Jun-305; Jun-306; Jun-307; Jun-308; Jun-310; Jun-311; Jun-312; Jun-313; Jun-314; Jun-315; Jun-316; Jun-317; Jun-318; Jun-319; Jun-320; Jun-321; Jun-322; Jun-323; Jun-324; Jun-325; Jun-326; Jun-327; Jun-328; KUNASH1; KUNASH2; KUNASH3; KUNASH4; KUNASH5; KUNASH6; KUNASH7; KUNASH8; Modern analog technique (MAT); MOKH1; MOKH10; MOKH100; MOKH101; MOKH102; MOKH103; MOKH104; MOKH105; MOKH106; MOKH107; MOKH108; MOKH109; MOKH11; MOKH110; MOKH111; MOKH112; MOKH113; MOKH114; MOKH115; MOKH116; MOKH117; MOKH118; MOKH119; MOKH12; MOKH120; MOKH121; MOKH122; MOKH123; MOKH124; MOKH125; MOKH126; MOKH127; MOKH128; MOKH129; MOKH13; MOKH130; MOKH131; MOKH133; MOKH134; MOKH135; MOKH136; MOKH137; MOKH138; MOKH139; MOKH14; MOKH140; MOKH141; MOKH142; MOKH143; MOKH144; MOKH145; MOKH146; MOKH147; MOKH148; MOKH149; MOKH15; MOKH150; MOKH151; MOKH152; MOKH153; MOKH154; MOKH155; MOKH156; MOKH157; MOKH158; MOKH159; MOKH16; MOKH160; MOKH161; MOKH162; MOKH163; MOKH164; MOKH165; MOKH166; MOKH167; MOKH168; MOKH169; MOKH17; MOKH170; MOKH171; MOKH172; MOKH173; MOKH174; MOKH175; MOKH176; MOKH177; MOKH178; MOKH18; MOKH180; MOKH181; MOKH182; MOKH183; MOKH184; MOKH185; MOKH186; MOKH187; MOKH188; MOKH189; MOKH19; MOKH194; MOKH195; MOKH196; MOKH197; MOKH199; MOKH2; MOKH200; MOKH202; MOKH204; MOKH206; MOKH207; MOKH208; MOKH209; MOKH21; MOKH210; MOKH211; MOKH212; MOKH213; MOKH214; MOKH215; MOKH216; MOKH217; MOKH218; MOKH219; MOKH22; MOKH220; MOKH221; MOKH223; MOKH224; MOKH225; MOKH226; MOKH227; MOKH228; MOKH23; MOKH231; MOKH233; MOKH234; MOKH237; MOKH238; MOKH239; MOKH24; MOKH240; MOKH241; MOKH242; MOKH25; MOKH26; MOKH27; MOKH28; MOKH29; MOKH3; MOKH30; MOKH31; MOKH32; MOKH33; MOKH34; MOKH35; MOKH36; MOKH38; MOKH39; MOKH41; MOKH42; MOKH43; MOKH44; MOKH45; MOKH46; MOKH47; MOKH48; MOKH49; MOKH50; MOKH51; MOKH53; MOKH54; MOKH55; MOKH56; MOKH59; MOKH6; MOKH60; MOKH61; MOKH62; MOKH63; MOKH64; MOKH65; MOKH66; MOKH67; MOKH68; MOKH69; MOKH7; MOKH71; MOKH72; MOKH73; MOKH75; MOKH76; MOKH77; MOKH78; MOKH79; MOKH8; MOKH80; MOKH81; MOKH82; MOKH83; MOKH84; MOKH85; MOKH86; MOKH87; MOKH88; MOKH89; MOKH9; MOKH91; MOKH92; MOKH93; MOKH94; MOKH95; MOKH96; MOKH97; MOKH98; MOKH99; Number of analogues; Oku-013; Oku-014; Oku-015; Oku-016; Oku-017; Oku-018; Oku-019; Oku-020; Oku-021; Oku-022; Oku-023; Oku-024; Oku-025; Oku-026; Oku-027; Oku-028; Oku-029; Oku-030; Oku-031; Oku-035; Oku-036; Oku-037; Oku-038; Oku-039; Oku-040; Oku-041; Oku-042; Oku-043; Oku-044; Oku-045; Oku-046; Oku-047; Oku-048; Oku-051; Oku-052; Oku-053; Oku-054; Oku-055; Oku-056; Oku-057; Oku-058; Oku-059; Oku-060; Oku-061; Oku-062; Oku-063; Oku-064; Oku-065; Oku-066; Oku-067; Oku-068; Oku-069; Oku-070; Oku-071; Oku-072; Oku-073; Oku-074; Oku-075; Oku-076; Oku-077; Oku-078; Oku-079; Oku-080; Oku-081; Oku-082; Oku-083; Oku-084; Oku-085; Oku-086; Oku-087; Oku-088; Oku-089; Oku-090; Oku-091; Oku-092; Oku-093; Oku-094; Oku-095; Oku-096; Oku-097; Oku-098; Oku-099; Oku-100; Oku-101; Oku-102; Oku-103; Oku-105; Oku-106; Oku-107; Oku-108; Oku-109; Oku-110; Oku-111; Oku-112; Pav_1; Pav_10; Pav_11; Pav_12; Pav_13a; Pav_13b; Pav_14; Pav_15; Pav_16; Pav_17; Pav_18; Pav_19; Pav_2; Pav_20; Pav_21; Pav_22; Pav_23; Pav_24; Pav_25; Pav_3a; Pav_3b; Pav_3c; Pav_3d; Pav_4a; Pav_4b; Pav_4c; Pav_5; Pav_6; Pav_7; Pav_8; Pav_9; Pav_H12-1; Pav_H13-1; Pav_H13-2; Pav_H13-2(2); Pav_H13-3; Pav_H14-1; Pav_H14-2; Pav_H17-1; Pav_H17-2; Pav_H19-1; Pav_H19-2; Pav_H19-3; Pav_H19-4; Pav_H19-4bis; Pav_H19-5; Pav_H19-6; Pav_H20-1; Pav_H20-2; Pav_H20-3; Pav_H20-4; Pav_H20-5; Pav_H20-6; Precipitation, annual mean; Precipitation, annual mean, maximum; Precipitation, annual mean, minimum; Precipitation, Apr-Sep; Precipitation, Apr-Sep, maximum; Precipitation, Apr-Sep, minimum; Precipitation, Oct-Mar; Precipitation, Oct-Mar, maximum; Precipitation, Oct-Mar, minimum; Russia; SAKH_01; SAKH_03; SAKH_04; SAKH_06; SAKH_08; SAKH_10; SAKH_11; SAKH_13; SAKH_15; SAKH_17; SAKH_19; SAKH_21; SAKH_23; SAKH_25; SAKH_26; SAKH_28; SAKH_29; SAKH_31; SAKH_33; SAKH_35; SAKH_36; SAKH_37; SAKH_39; SAKH_40; SAKH_41; SAKH_43; SAKH_45; SAKH_47; SAKH_49; SAKH_51; SAKH_53; SAKH_54; SAKH_55; SAKH_57; SAKH_58; SAKH_59; SAKH_61; SAKH_62; SAKH_63; Temperature, annual mean; Temperature, annual mean, maximum; Temperature, annual mean, minimum; Temperature, coldest month; Temperature, coldest month, maximum; Temperature, coldest month, minimum; Temperature, difference; Temperature, difference, maximum; Temperature, difference, minimum; Temperature, warmest month; Temperature, warmest month, maximum; Temperature, warmest month, minimum; Temperature coldness index; Temperature coldness index, maximum; Temperature coldness index, minimum; Temperature warmth index; Temperature warmth index, maximum;
    Type: Dataset
    Format: text/tab-separated-values, 22316 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 5
    facet.materialart.
    Unknown
    (Table S2) Reference pollen dataset of 798 modern surface spectra (2011)
    PANGAEA
    Details
    Publication Date: 2024-03-06
    Keywords: Abies; Acer; Aesculus; Alnus; AMUR1; AMUR10; AMUR11; AMUR12; AMUR13; AMUR14; AMUR15; AMUR16; AMUR17; AMUR18; AMUR19; AMUR2; AMUR20; AMUR21; AMUR22; AMUR23; AMUR24; AMUR25; AMUR26; AMUR27; AMUR28; AMUR29; AMUR3; AMUR31; AMUR32; AMUR33; AMUR34; AMUR35; AMUR36; AMUR37; AMUR38; AMUR39; AMUR4; AMUR40; AMUR43; AMUR44; AMUR45; AMUR46; AMUR47; AMUR48; AMUR49; AMUR5; AMUR50; AMUR51; AMUR52; AMUR53; AMUR54; AMUR55; AMUR56; AMUR57; AMUR6; AMUR7; AMUR8; AMUR9; Betula; Camellia; Carpinus; Castanopsis; China; Corylus; Counting, palynology; Cryptomeria; DEPTH, sediment/rock; Elevation of event; Ericaceae; Event label; Fagus; Fraxinus; Hand corer; HCOR; HOKK_02; HOKK_05; HOKK_07; HOKK_08; HOKK_10; HOKK_11; HOKK_14; Ilex; Japan; Jss-001; Jss-002; Jss-003; Jss-004; Jss-005; Jss-006; Jss-007; Jss-008; Jss-009; Jss-010; Jss-011; Jss-012; Jss-013; Jss-014; Jss-015; Jss-016; Jss-017; Jss-018; Jss-019; Jss-020; Jss-021; Jss-022; Jss-023; Jss-024; Jss-025; Jss-026; Jss-027; Jss-028; Jss-029; Jss-030; Jss-031; Jss-032; Jss-033; Jss-034; Jss-035; Jss-036; Jss-037; Jss-038; Jss-039; Jss-040; Jss-041; Jss-042; Jss-043; Jss-044; Jss-045; Jss-046; Jss-047; Jss-048; Jss-049; Jss-050; Jss-051; Jss-052; Jss-053; Jss-054; Jss-055; Jss-056; Jss-057; Jss-058; Jss-059; Jss-060; Jss-061; Jss-062; Jss-063; Jss-064; Jss-065; Jss-066; Jss-067; Jss-068; Jss-069; Jss-070; Jss-071; Jss-072; Jss-073; Jss-074; Jss-075; Jss-076; Jss-077; Jss-078; Jss-079; Jss-080; Jss-081; Jss-082; Jss-083; Jss-084; Jss-085; Jss-086; Jss-087; Jss-088; Jss-089; Jss-090; Jss-091; Jss-092; Jss-093; Jss-094; Jss-095; Jss-096; Jss-097; Jss-098; Jss-099; Jss-100; Jss-101; Jss-102; Jss-103; Jss-104; Jss-105; Jss-106; Jss-107; Jss-108; Jss-109; Jss-110; Jss-111; Jss-112; Jss-113; Jss-114; Jss-115; Jss-116; Jss-117; Jss-118; Jss-119; Jss-120; Jss-121; Jss-122; Jss-123; Jss-124; Jss-125; Jss-126; Jss-127; Jss-128; Jss-129; Jss-130; Jss-131; Jss-132; Jss-133; Jss-134; Jss-135; Jss-136; Jss-137; Jss-138; Jss-139; Jss-140; Jss-141; Jss-142; Jss-143; Jss-144; Jss-145; Jss-146; Jss-147; Jss-148; Jss-149; Jss-150; Jss-151; Jss-152; Jss-153; Jss-154; Jss-155; Jss-156; Jss-157; Jss-158; Jss-159; Jss-160; Jss-161; Jss-162; Jss-163; Jss-164; Jss-165; Jss-166; Jss-167; Jss-168; Jss-169; Jss-170; Jss-171; Jss-172; Jss-173; Jss-174; Jss-175; Jss-176; Jss-177; Jss-178; Jss-179; Jss-180; Jss-181; Jss-182; Jss-183; Jss-184; Jss-185; Jss-186; Jss-187; Jss-188; Jss-189; Jss-190; Jss-191; Jss-192; Jss-193; Jss-194; Jss-195; Jss-196; Jss-197; Jss-198; Jss-199; Jss-200; Jss-201; Jss-202; Jss-203; Jss-204; Jss-205; Jss-206; Jss-207; Jss-208; Jss-209; Jss-210; Jss-211; Jss-212; Jss-213; Jss-214; Jss-215; Jss-216; Jss-217; Jss-218; Jss-219; Jss-220; Jss-221; Jss-222; Jss-223; Jss-224; Jss-225; Jss-226; Jss-227; Jss-228; Jss-229; Jss-230; Jss-231; Jss-232; Jss-233; Jss-234; Jss-235; Jss-236; Jss-237; Jss-238; Jss-239; Jss-240; Jss-241; Jss-242; Jss-243; Jss-244; Jss-245; Jss-246; Jss-247; Jss-248; Jss-249; Jss-250; Jss-251; Jss-252; Jss-253; Jss-254; Jss-255; Jss-256; Jss-257; Jss-258; Jss-259; Jss-260; Jss-261; Jss-262; Jss-263; Jss-264; Jss-265; Jss-266; Jss-267; Jss-268; Jss-269; Jss-270; Jss-271; Jss-272; Jss-273; Jss-274; Jss-275; Jss-276; Jss-277; Jss-278; Jss-279; Jss-280; Jss-281; Jss-282; Jss-283; Jss-284; Jss-285; Juglans; Jun-286; Jun-287; Jun-288; Jun-289; Jun-290; Jun-291; Jun-292; Jun-293; Jun-294; Jun-295; Jun-296; Jun-297; Jun-298; Jun-299; Jun-300; Jun-301; Jun-302; Jun-303; Jun-304; Jun-305; Jun-306; Jun-307; Jun-308; Jun-310; Jun-311; Jun-312; Jun-313; Jun-314; Jun-315; Jun-316; Jun-317; Jun-318; Jun-319; Jun-320; Jun-321; Jun-322; Jun-323; Jun-324; Jun-325; Jun-326; Jun-327; Jun-328; KUNASH1; KUNASH2; KUNASH3; KUNASH4; KUNASH5; KUNASH6; KUNASH7; KUNASH8; Larix; Latitude of event; Longitude of event; MOKH1; MOKH10; MOKH100; MOKH101; MOKH102; MOKH103; MOKH104; MOKH105; MOKH106; MOKH107; MOKH108; MOKH109; MOKH11; MOKH110; MOKH111; MOKH112; MOKH113; MOKH114; MOKH115; MOKH116; MOKH117; MOKH118; MOKH119; MOKH12; MOKH120; MOKH121; MOKH122; MOKH123; MOKH124; MOKH125; MOKH126; MOKH127; MOKH128; MOKH129; MOKH13; MOKH130; MOKH131; MOKH133; MOKH134; MOKH135; MOKH136; MOKH137; MOKH138; MOKH139; MOKH14; MOKH140; MOKH141; MOKH142; MOKH143; MOKH144; MOKH145; MOKH146; MOKH147; MOKH148; MOKH149; MOKH15; MOKH150; MOKH151; MOKH152; MOKH153; MOKH154; MOKH155; MOKH156; MOKH157; MOKH158; MOKH159; MOKH16; MOKH160; MOKH161; MOKH162; MOKH163; MOKH164; MOKH165; MOKH166; MOKH167; MOKH168; MOKH169; MOKH17; MOKH170; MOKH171; MOKH172; MOKH173; MOKH174; MOKH175; MOKH176; MOKH177; MOKH178; MOKH18; MOKH180; MOKH181; MOKH182; MOKH183; MOKH184; MOKH185; MOKH186; MOKH187; MOKH188; MOKH189; MOKH19; MOKH194; MOKH195; MOKH196; MOKH197; MOKH199; MOKH2; MOKH200; MOKH202; MOKH204; MOKH206; MOKH207; MOKH208; MOKH209; MOKH21; MOKH210; MOKH211; MOKH212; MOKH213; MOKH214; MOKH215; MOKH216; MOKH217; MOKH218; MOKH219; MOKH22; MOKH220; MOKH221; MOKH223; MOKH224; MOKH225; MOKH226; MOKH227; MOKH228; MOKH23; MOKH231; MOKH233; MOKH234; MOKH237; MOKH238; MOKH239; MOKH24; MOKH240; MOKH241; MOKH242; MOKH25; MOKH26; MOKH27; MOKH28; MOKH29; MOKH3; MOKH30; MOKH31; MOKH32; MOKH33; MOKH34; MOKH35; MOKH36; MOKH38; MOKH39; MOKH40; MOKH41; MOKH42; MOKH43; MOKH44; MOKH45; MOKH46; MOKH47; MOKH48; MOKH49; MOKH50; MOKH51; MOKH53; MOKH54; MOKH55; MOKH56; MOKH59; MOKH6; MOKH60; MOKH61; MOKH62; MOKH63; MOKH64; MOKH65; MOKH66; MOKH67; MOKH68; MOKH69; MOKH7; MOKH71; MOKH72; MOKH73; MOKH75; MOKH76; MOKH77; MOKH78; MOKH79; MOKH8; MOKH80; MOKH81; MOKH82; MOKH83; MOKH84; MOKH85; MOKH86; MOKH87; MOKH88; MOKH89; MOKH9; MOKH91; MOKH92; MOKH93; MOKH94; MOKH95; MOKH96; MOKH97; MOKH98; MOKH99; Myrica; Oku-013; Oku-014; Oku-015; Oku-016; Oku-017; Oku-018; Oku-019; Oku-020; Oku-021; Oku-022; Oku-023; Oku-024; Oku-025; Oku-026; Oku-027; Oku-028; Oku-029; Oku-030; Oku-031; Oku-035; Oku-036; Oku-037; Oku-038; Oku-039; Oku-040; Oku-041; Oku-042; Oku-043; Oku-044; Oku-045; Oku-046; Oku-047; Oku-048; Oku-051; Oku-052; Oku-053; Oku-054; Oku-055; Oku-056; Oku-057; Oku-058; Oku-059; Oku-060; Oku-061; Oku-062; Oku-063; Oku-064; Oku-065; Oku-066; Oku-067; Oku-068; Oku-069; Oku-070; Oku-071; Oku-072; Oku-073; Oku-074; Oku-075; Oku-076; Oku-077; Oku-078; Oku-079; Oku-080; Oku-081; Oku-082; Oku-083; Oku-084; Oku-085; Oku-086; Oku-087; Oku-088; Oku-089; Oku-090; Oku-091; Oku-092; Oku-093; Oku-094; Oku-095; Oku-096; Oku-097; Oku-098; Oku-099; Oku-100; Oku-101; Oku-102; Oku-103; Oku-105; Oku-106; Oku-107; Oku-108; Oku-109; Oku-110; Oku-111; Oku-112; Pav_1; Pav_10; Pav_11; Pav_12; Pav_13a; Pav_13b; Pav_14; Pav_15; Pav_16; Pav_17; Pav_18; Pav_19; Pav_2; Pav_20; Pav_21; Pav_22; Pav_23; Pav_24; Pav_25; Pav_3a; Pav_3b; Pav_3c; Pav_3d; Pav_4a; Pav_4b; Pav_4c; Pav_5; Pav_6; Pav_7; Pav_8; Pav_9; Pav_H12-1; Pav_H13-1; Pav_H13-2; Pav_H13-2(2); Pav_H13-3; Pav_H14-1; Pav_H14-2; Pav_H17-1; Pav_H17-2; Pav_H19-1; Pav_H19-2; Pav_H19-3; Pav_H19-4; Pav_H19-4bis; Pav_H19-5; Pav_H19-6; Pav_H20-1; Pav_H20-2; Pav_H20-3; Pav_H20-4; Pav_H20-5; Pav_H20-6; Picea; Pinus; Podocarpus; Quercus, deciduous; Quercus evergreen; Reference/source; Rhododendron; Rhus; Russia; SAKH_01; SAKH_03; SAKH_04; SAKH_06; SAKH_08; SAKH_10; SAKH_11; SAKH_13; SAKH_15; SAKH_17; SAKH_19; SAKH_21; SAKH_23; SAKH_25; SAKH_26; SAKH_28; SAKH_29; SAKH_31; SAKH_33; SAKH_35; SAKH_36; SAKH_37; SAKH_39; SAKH_40; SAKH_41; SAKH_43; SAKH_45; SAKH_47; SAKH_49; SAKH_51; SAKH_53; SAKH_54; SAKH_55; SAKH_57; SAKH_58; SAKH_59; SAKH_61; SAKH_62; SAKH_63; Salix; Sciadopitys; Symplocos; Taxodiaceae; Tilia; Tsuga; Ulmus; Viburnum
    Type: Dataset
    Format: text/tab-separated-values, 26334 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 6
    facet.materialart.
    Unknown
    CLAM age model and microcharcoal of sediment core BIW95-4 (2017)
    PANGAEA
    Details
    Publication Date: 2024-04-20
    Keywords: Abrupt Climate Changes and Environmental Responses; Accumulation model; ACER; BIW95-4; Calendar age; Calendar age, maximum/old; Calendar age, minimum/young; Charcoal; Classical age-modeling approach, CLAM (Blaauw, 2010); DEPTH, sediment/rock; Lake Biwa; Sample ID; Type of age model; Unit
    Type: Dataset
    Format: text/tab-separated-values, 455 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 7
    facet.materialart.
    Unknown
    CLAM age model and pollen profile of sediment core BIW95-4 (2017)
    PANGAEA
    Details
    Publication Date: 2024-04-20
    Keywords: Abies; Abrupt Climate Changes and Environmental Responses; Accumulation model; Acer; ACER; Aesculus; Alisma; Alnus; Amaranthaceae/Chenopodiaceae; Anemone; Apiaceae; Araliaceae; Artemisia; Asteraceae; Betula; BIW95-4; Brassicaceae; Buxus; Calendar age; Calendar age, maximum/old; Calendar age, minimum/young; Carpinus/Ostrya; Carpinus tschonoskii; Caryophyllaceae; Castanea/Castanopsis; Celastraceae; Celtis/Aphananthe; Cercidiphyllum; Classical age-modeling approach, CLAM (Blaauw, 2010); Cornus; Corylus; Counting, palynology; Cryptomeria; Cupressaceae-type; Cyperaceae; DEPTH, sediment/rock; Elaeagnaceae; Equisetum; Ericaceae; Eriocaulon; Fagus crenata; Fagus japonica; Fraxinus; Gentiana; Haloragis/Myriophyllum; Hemiptelea; Ilex; Impatiens; Isoetes; Juglans/Pterocarya; Lake Biwa; Lamiaceae; Larix; Ligustrum; Liliaceae; Lonicera; Lycopodium clavatum-type; Lycopodium inundatum-type; Lycopodium serratum-type; Lysichiton; Lythrum; Menyanthes; Myrica; Nuphar; Nymphoides; Nymphoides indica; Osmundaceae; Parthenocissus; Phellodendron; Picea; Pinus; Poaceae; Pollen indeterminata; Polygonum persicaria-type; Polygonum reynoutria-type; Polypodiales; Potamogeton; Pteridium; Pteridophyta; Quercus subgen. Cyclobalanopsis; Quercus subgen. Lepidobalanus; Ranunculus; Rhamnaceae; Rhus; Rosaceae; Rutaceae; Sagittaria; Salix; Sample ID; Sanguisorba; Sciadopitys; Sparganium/Trapa; Sparganium/Typha; Sphagnum; Styracaceae; Symplocos; Thalictrum; Tilia; Tsuga; Type of age model; Ulmus/Zelkova; Viburnum; Vitis
    Type: Dataset
    Format: text/tab-separated-values, 11013 data points
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  • 8
    Electronic Resource
    Electronic Resource
    Quaternary vertical offset and average slip rate of the Nojima Fault on Awaji Island, Japan (2001)
    Melbourne, Australia : Blackwell Science Pty
    The @island arc 10 (2001), S. 0 
    Details
    ISSN: 1440-1738
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Abstract Drilling was carried out to penetrate the Nojima Fault where the surface rupture occurred associated with the 1995 Hyogo-ken Nanbu earthquake. Two 500 m boreholes were successfully drilled through the fault zone at a depth of 389.4 m. The drilling data show that the relative uplift of the south-east side of the Nojima Fault (south-west segment) was approximately 230 m. The Nojima branch fault, which branches from the Nojima Fault, is inferred to extend to the Asano Fault. From the structural contour map of basal unconformity of the Kobe Group, the vertical component of displacement of the Nojima branch–Asano Fault is estimated to be 260–310 m. Because the vertical component of displacement on the Nojima Fault of the north-east segment is a total of those of the Nojima Fault of the south-west segment and of the Nojima branch–Asano Fault, it is estimated to total to 490–540 m. From this, the average vertical component of the slip rate on the Nojima Fault is estimated to be 0.4–0.45 m/103 years for the past 1.2 million years.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1440-1738.2001.00334.x
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  • 9
    Electronic Resource
    Electronic Resource
    Thermal anomaly around the Nojima Fault as detected by fission-track analysis of Ogura 500 m borehole samples (2001)
    Melbourne, Australia : Blackwell Science Pty
    The @island arc 10 (2001), S. 0 
    Details
    ISSN: 1440-1738
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Abstract To better understand heat generation and transfer along earthquake faults, this paper presents preliminary zircon fission-track (FT) length data from the Nojima Fault, Awaji Island, Japan, which was activated during the 1995 Kobe earthquake (Hyogo-ken Nanbu earthquake). Samples were collected of Cretaceous granitic rocks from the Ogura 500 m borehole as well as at outcrops adjacent to the borehole site. The Nojima Fault plane was drilled at a depth of 389.4 m (borehole apparent depth). Fission-track lengths in zircons from localities 〉 60 m distance from the fault plane, as well as those from outcrops, are characterized by the mean values of ≈10–11 μm and unimodal distributions with positive skewness, which show no signs of an appreciable reduction in FT length. In contrast, those from nearby the fault at depths show significantly reduced mean track lengths of ≈6–8 μm and distributions having a peak around 6–7 μm with rather negative skewness. In conjunction with other geological constraints, these results are best interpreted by a recent thermal anomaly around the fault, which is attributable to heat transfer via focused fluids from the deep interior of the crust and/or heat dispersion via fluids associated with frictional heating by fault motion.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1440-1738.2001.00344.x
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  • 10
    Electronic Resource
    Electronic Resource
    Paleogene and Plio-Pleistocene basin formation around northwestern Kyushu, Japan (1999)
    Melbourne, Australia : Blackwell Science Pty
    The @island arc 8 (1999), S. 0 
    Details
    ISSN: 1440-1738
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Cenozoic basin-forming processes in northwestern Kyushu were studied on the basis of geological and geophysical data. Gravity anomaly analysis delineated four sedimentary basins in the study area: Goto-nada, Nishisonogi, Amakusa-nada, and Shimabara. Borehole stratigraphy and reflection seismic interpretation suggest that the Goto-nada Basin was subdivided into the Paleogene and Plio-Pleistocene depocenters (Goto-nada 1 and 2). In the Paleogene, Amakusa-nada Basin was rapidly subsiding together with the Shimabara Basin as part of a large graben. Goto-nada 1 and Nishisonogi basins belonged to another depositional area. After stagnant subsidence stage in the early Miocene, the study area became a site of basaltic activity (since 10 Ma) and vigorous subsidence in the Plio-Pleistocene. Goto-nada 2 Basin is accompanied with numerous east–west active faults, and separated from the Amakusa-nada Basin by a northeast– southwest basement high, Nomo Ridge. Plio-Pleistocene subsidence of the Amakusa-nada Basin is related with low-angle normal faulting on the eastern flank of the Nomo Ridge. Shimabara Basin is a composite volcano-tectonic depression which is studded by east–west faults. Focal mechanism on active faults suggests transtensional stress regime in the study area.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1046/j.1440-1738.1999.00223.x
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