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  • 1
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Barth, Aaron M; Clark, Peter U; Bill, Nicholas S; He, Feng; Pisias, Nicklas G (2018): Climate evolution across the Mid-Brunhes Transition. Climate of the Past, 14(12), 2071-2087, https://doi.org/10.5194/cp-14-2071-2018
    Publikationsdatum: 2024-06-18
    Beschreibung: The Mid-Brunhes Transition (MBT) began ∼430ka with an increase in the amplitude of the 100-kyr climate cycles of the past 800,000 years. The MBT has been identified in ice-core records, which indicate interglaciations became warmer with higher atmospheric CO2 levels after the MBT, and benthic oxygen isotope (δ18O) records, which suggest that post-MBT interglaciations had higher sea levels than pre-MBT interglaciations. It remains unclear, however, whether the MBT was a globally synchronous phenomenon that included other components of the climate system. Here we further characterize changes in the climate system across the MBT through statistical analyses of ice-core and δ18O records as well as sea-surface temperature, benthic carbon isotope, and dust accumulation records. Our results demonstrate that the MBT was a global event with a significant increase in climate variance in most components of the climate system assessed here. However, our results indicate that the onset of high-amplitude variability in temperature, atmospheric CO2, and sea level at ∼430ka was preceded by changes in the carbon cycle, ice sheets, and monsoon strength during MIS 14 and 13.
    Materialart: Dataset
    Format: application/zip, 3 datasets
    Standort Signatur Erwartet Verfügbarkeit
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  • 2
    Publikationsdatum: 2024-06-18
    Schlagwort(e): DATE/TIME; DEPTH, water; File format; File name; File size; JPI Oceans - Ecological Aspects of Deep-Sea Mining; JPIO-MiningImpact; LATITUDE; LONGITUDE; MULT; Multiple investigations; SO239; SO239-track; Sonne_2; Swath-mapping system Simrad EM122 (Kongsberg Maritime AS); Uniform resource locator/link to raw data file
    Materialart: Dataset
    Format: text/tab-separated-values, 1120 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 3
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Ceccopieri, Milena; Carreira, Renato S; Wagener, Angela L R; Hefter, Jens; Mollenhauer, Gesine (2018): On the application of alkenone- and GDGT-based temperature proxies in the south-eastern Brazilian continental margin. Organic Geochemistry, 126, 43-56, https://doi.org/10.1016/j.orggeochem.2018.10.009
    Publikationsdatum: 2024-06-18
    Beschreibung: The applicability of two organic geochemical proxies (UK'37 based on alkenones and TEXH86 based on glycerol dialkyl glycerol tetraethers) for ocean temperatures was investigated on a regional scale in the SE Brazilian continental margin (Campos Basin) using 53 core-top sediments. In 71% of the samples for UK'37 and 85% for TEXH86, the estimated annual mean sea surface temperature (SST) is comparable to the climatological annual mean data, with deviations within the calibration error. The surface TEXH86 estimates reflects the surface mixed layer, while the depth-integrated (0-200 m) TEXH86 estimates showed better agreement with temperatures at 100-200 mdepth. In addition, the SST-UK'37 results were more consistent (73% of the samples) using a winter calibration rather than an annual mean calibration. This seasonal effect might be ascribed to an increase in the abundance of haptophytes in the region during the winter. Exceptions to these general trends were observed for both proxies as a strong cold bias in reconstructed temperature in a few samples in the southern portion of the studied region, which may be related to (i) a predominant subsurface habitat of Thaumarchaeota combined with enhanced primary production and flux of particles during upwelling and (ii) alkenones being laterally transported from adjacent colder waters. Effects of river input of terrestrially sourced GDGTs on TEXH86 are not evident. Overall, our findings show that UK'37 and TEXH86 are suitable temperature proxies for paleoclimate studies at a regional scale in the SE Brazilian continental margin, but on a local scale the effects of upwelling must be taken in consideration.
    Schlagwort(e): A01; A02; A03; A04; A05; A06; A07; A08; A09; A10; A11; A12; Acyclic glycerol dialkyl glycerol tetraether, fractional abundance; Alkenone, per unit mass total organic carbon; Alkenone, unsaturation index UK'37; Alkenone per unit sediment mass; B1; B10; B11; B12; B2; B3; B4; B5; B6; B7; B8; B9; BCM; Box corer, modified; Cabo Frio upwelling system; Campos Basin; Campos Basin Environmental Heterogeneity Project (CENPES/Petrobras); Crenarchaeol, fractional abundance; Crenarchaeol isomer, fractional abundance; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Dicyclic glycerol dialkyl glycerol tetraether, fractional abundance; Event label; extracted from the World Ocean Atlas 2013 (WOA13); G03; G04; G05; G07; G08; G09; G10; G11; G12; Gyre; H1; H10; H11; H12; H2; H3; H4; H5; H6; H7; HAB_A01; HAB_A02; HAB_A03; HAB_A04; HAB_A05; HAB_A06; HAB_A07; HAB_A08; HAB_A09; HAB_A10; HAB_A11; HAB_A12; HAB_B1; HAB_B10; HAB_B11; HAB_B12; HAB_B2; HAB_B3; HAB_B4; HAB_B5; HAB_B6; HAB_B7; HAB_B8; HAB_B9; HAB_G03; HAB_G04; HAB_G05; HAB_G07; HAB_G08; HAB_G09; HAB_G10; HAB_G11; HAB_G12; HAB_H1; HAB_H10; HAB_H11; HAB_H12; HAB_H2; HAB_H3; HAB_H4; HAB_H5; HAB_H6; HAB_H7; HAB_I02; HAB_I04; HAB_I05; HAB_I06; HAB_I07; HAB_I08; HAB_I09; HAB_I10; HAB_I11; HAB_I12; HAB10; HAB11; HAB13; HAB5; HAB8; HAB9; Habitats; High Performance Liquid Chromatography (HPLC-APCI-MS); I02; I04; I05; I06; I07; I08; I09; I10; I11; I12; Isoprenoid glycerol dialkyl glycerol tetraether, per unit mass total organic carbon; Isoprenoid glycerol dialkyl glycerol tetraether, per unit sediment mass; Miss Emma McCall; Monocyclic glycerol dialkyl glycerol tetraether, fractional abundance; Sea surface temperature, annual mean; South Atlantic Ocean; Surface sediments; Tetraether index of 86 carbon atoms; TEXH86; Tricyclic glycerol dialkyl glycerol tetraether, fractional abundance; UK'37; van Veen Grab, modified; VGRABM
    Materialart: Dataset
    Format: text/tab-separated-values, 745 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 4
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Murphy, Conor; Broderick, Ciaran; Burt, Timothy P; Curley, Mary; Duffy, Catriona; Hall, Julia; Harrigan, Shaun; Matthews, Tom K R; Macdonald, Neil; McCarthy, Gerard D; McCarthy, Mark P; Mullan, Donal; Noone, Simon; Osborn, Timothy J; Ryan, Ciara; Sweeney, John; Thorne, Peter W; Walsh, Seamus; Wilby, Robert L (2017): A 305-year continuous monthly rainfall series for the Island of Ireland (1711-2016). Climate of the Past Discussions, 14(1), 1-39, https://doi.org/10.5194/cp-2017-142
    Publikationsdatum: 2024-06-18
    Beschreibung: This dataset provides a continuous monthly rainfall series for the Island of Ireland commencing in January 1711 and running to December 2016. It draws upon diverse sources including weather diaries and early observations. The early record has been quality assured (so far as is possible), through comparison with other long term observational records and climate reconstructions for the regions of the British Irish Isles.
    Schlagwort(e): DATE/TIME; Ireland; Is_of_Ireland; Precipitation, monthly total
    Materialart: Dataset
    Format: text/tab-separated-values, 3672 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 5
    Publikationsdatum: 2024-06-18
    Beschreibung: Regional stacks of benthic carbon isotopes from previously published data for the shallow North Atlantic (〈 2000 m), deep North Atlantic (〉 2000 m), and the South Atlantic for the last 800 kyr. Gradients between the shallow and deep North Atlantic, and between the deep North Atlantic and the South Atlantic.
    Materialart: Dataset
    Format: application/vnd.openxmlformats-officedocument.spreadsheetml.sheet, 92.3 kBytes
    Standort Signatur Erwartet Verfügbarkeit
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  • 6
    Publikationsdatum: 2024-06-18
    Schlagwort(e): 162-983; Age, maximum/old; Age, minimum/young; Age model; COMPCORE; Composite Core; DEPTH, sediment/rock; Joides Resolution; Leg162; South Atlantic Ocean
    Materialart: Dataset
    Format: text/tab-separated-values, 4830 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 7
    Publikationsdatum: 2024-06-18
    Schlagwort(e): 0016PG; 0021PG; 0026PG; 0032PG; 0036PG; 0038PG; 0044PG; 0050PG; 0055PG; 0058PG; 0066PG; 0071PG; 0075PG; 0082PG; 0091PG; 108-658; 130-807A; 138-846; 154-928; 162-980; 162-982; 162-983; 162-984; 177-1088B; 177-1089; 177-1090; 184-1143; 293; 303-U1308; 311; 52-43; 68-502; 90b; Agadir Canyon; ANT-XI/2; Arabian Sea; Atlantic Ocean; BIGSET; Biscaya; Brazil Basin; BT4; CALYPSO; Calypso Corer; Calypso Square Core System; Canarias Sea; Cape Basin; Caribbean Sea/RIDGE; CASQS; CH73-139; CH73-139C; CH7X; CH8X; Chatham Rise; CHN115-70PC; CHN82-24; Comment; COMPCORE; Composite Core; DRILL; Drilling/drill rig; East Atlantic; ELEVATION; EN06601; EN066-16PG; EN066-21PG; EN066-26PG; EN066-32PG; EN066-36PG; EN066-38PG; EN066-44PG; Endeavor; Event label; EW9209-1JPC; EW9504-05PC; Exp303; FR01/97; FR01/97-12; Franklin; GC; GeoB1041; GeoB1101-4; GeoB1112-3; GeoB1117-2; GeoB1118; GeoB1211; GeoB1214-1; GeoB1710-3; GeoB3004-1; GeoB3104-1; GeoB4216-1; GeoB4240-2; GeoB6718-2; GeoB7920-2; GeoB9508-5; GeoB9526-5; GEOFAR; GEOTROPEX 83, NOAMP I; GGC; Giant box corer; Giant gravity corer; Giant piston corer; GIK11944-2; GIK12328-5; GIK12347-2; GIK12379-3; GIK12392-1; GIK13521-1; GIK15612-2; GIK15666-6; GIK15669-1; GIK15672; GIK16004-1; GIK16006-1; GIK16017; GIK16030-1; GIK16402; GIK16415; GIK17049-6; GIK17050-1; GIK17051; GIK17055-1; GIK17961-2; GIK23414-9; GIK23415-9; GIK23416-4; GIK23417-1; GIK23418-8; GIK23419-8; GIK23519-5; GKG; Glomar Challenger; GPC; Gravity corer; Gravity corer (Kiel type); Greenland Sea; Guinea Basin; Gulf of Aden; Hakurei-Maru No.2 (1980); HM52-43; IMAGES I; IMAGES II; IMAGES III - IPHIS; IMAGES V; IMAGES VII - WEPAMA; IMAGES XV - Pachiderme; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Jean Charcot; Joides Resolution; JOPSII-6; JPC; Jumbo Piston Core; KAL; Kasten corer; KF13; KL-74, AS-12; KN11002; KN159-5; Knorr; KNR110-50; KNR110-55; KNR110-58; KNR110-66; KNR110-71; KNR110-75; KNR110-82; KNR110-91; KNR159-17; KNR159-20; KNR159-33; KNR159-36; KNR159-42; KNR159-5; KNR159-5-125GGC; KNR159-5 17JPC; KNR159-5-22GGC; KNR159-5 30GGC; KNR159-5-30GGC; KNR159-5-33GGC; KNR159-5-36GGC; KNR159-5-63GGC; KNR159-5-78GGC; KNR159-5 90GGC; KNR159-63; KNR159-90; KOL; LATITUDE; Leg108; Leg130; Leg138; Leg154; Leg162; Leg177; Leg184; Leg68; Le Noroit; Le Suroît; LONGITUDE; M11/1; M12/1; M12392-1; M17/2; M20/2; M23; M23_099; M23414; M25; M31/3; M31/3-107_GC; M35/1; M35003-4; M37/1; M39; M53; M53_166; M53_169; M53_172-1; M53/1; M57; M6/6; M60; M65; M65/1; M9/4; Marion Dufresne (1995); MD012378; MD01-2378; MD07-3076; MD07-3076Q; MD101; MD105; MD106; MD114; MD122; MD159; MD952039; MD95-2039; MD952040; MD95-2040; MD96-2080; MD962080, ABS; MD972120; MD97-2120; MD972151; MD97-2151; MD99-2334; Meteor (1964); Meteor (1986); MONITOR MONSUN; N414NGC102; NA87-22; Namibia continental slope; NE-Brazilian continental margin; NH95-1; NH95-1_N414; Nordost-Atlantik-Expedition 1971; North Atlantic; North Atlantic Climate 1; Northeast Atlantic; Northeast Pacific; northern North Atlantic; Norwegian Sea; OCE205-103GGC; OCE205-2-103GGC; Ocean and sea region; off West Africa; Orgon4-KS8; PALEOCINAT; PC; Persistent Identifier; Piston corer; Piston corer (Kiel type); Polarstern; Porcupine Seabight; Porto Seamount; POS210/2; POS265; POS478-2; Poseidon; PS2498-1; PS28; PS28/304; RC13; RC13-110; RC13-114; RC13-228; RC16; RC16-119; RC16-84; Reference/source; Robert Conrad; Sample code/label; SL; SO42; SO42-74KL; SO95; Sonne; South Atlantic; South Atlantic Ocean; South China Sea; Southern Agulhas Bank; South Pacific Ocean; Southwest Pacific; SPC; Sphincter corer; SU90-03; SU90-39; SUBTROPEX 82; Timor Sea; Uniform resource locator/link to reference; V19; V19-27; V22; V22-197; V23; V23-81; V24; V24-109; V24-253; V25; V25-59; V28; V28-127; V28-14; V29; V29-135; V29-202; V30; V30-40; V30-49; Vema; Vema Channel; Victor Hensen; Walvis Ridge; West equatorial Pacific Ocean; Western Atlantic
    Materialart: Dataset
    Format: text/tab-separated-values, 469 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 8
    Publikationsdatum: 2024-06-18
    Beschreibung: Rapid changes in ocean circulation and climate have been observed in marine-sediment and ice cores over the last glacial period and deglaciation, highlighting the non-linear character of the climate system and underlining the possibility of rapid climate shifts in response to anthropogenic greenhouse gas forcing. To date, these rapid changes in climate and ocean circulation are still not fully explained. One obstacle hindering progress in our understanding of the interactions between past ocean circulation and climate changes is the difficulty of accurately dating marine cores. Here, we present a set of 92 marine sediment cores from the Atlantic Ocean for which we have established age-depth models that are consistent with the Greenland GICC05 ice core chronology, and computed the associated dating uncertainties, using a new deposition modeling technique. This is the first set of consistently dated marine sediment cores enabling paleoclimate scientists to evaluate leads/lags between circulation and climate changes over vast regions of the Atlantic Ocean. Moreover, this data set is of direct use in paleoclimate modeling studies.
    Schlagwort(e): 053-2; 057-1; 087-1; 162-983; 165-1002; 172-1060; 175-1078C; 175-1084; 293; 311; 3664N/S; 63F/NL; 90b; 94-609; Agadir Canyon; ALIENOR; ALTITUDE; AMADEUS; Amazon Fan; AMOCINT, IMAGES XVII; Angola Basin; ARK-X/2; Atlantic; Atlantic Ocean; Atlantic sediment cores; Azores; BC; Benguela Current, South Atlantic Ocean; Blake-Bahama Outer Ridge, North Atlantic Ocean; Box corer; CALYPSO; Calypso Corer; Calypso square corer; Calypso Square Core System; CASQ; CASQS; Cayman Rise, Caribbean Sea; CD159; CD159-10; CD159-17; CEPAG; CH22KW31; CH69-K09; Charles Darwin; CHO288-54; Comment; COMPCORE; Composite Core; consistent dating; Continental Slope Northeast Brazil; Core; CORE; Corner Rise; DAPC2; Denmark Strait; De Soto Canyon; DRILL; Drilling/drill rig; East Atlantic; ENAM9321; ENAM93-21; Event label; EW9209-1JPC; Faeroes Bank; Falkland Plateau, Southern Falkland Plateau (same site as GC526); Faroe Islands margin; Florida Strait; French Guiana; GC; GC528 CORE_NO 528; GeoB1023-5; GeoB1515-1; GeoB16202-2; GeoB16206-1; GeoB16224-1; GeoB1711; GeoB1711-4; GeoB1720-2; GeoB3202-1; GeoB3910-2; GeoB4240-2; GeoB5546-2; GeoB6201-5; GeoB7920-2; GeoB9508-5; GeoB9526-5; GEOFAR; GEOSCIENCES, MARMARCORE; GGC; GGC5; Giant gravity corer; GIK12392-1; GIK15669-1; GIK23415-9; GL1090; GL-1090; Glomar Challenger; Gravity corer; Gravity corer (Kiel type); GS07-150-17/1GC-A; Iceland; IMAGES I; IMAGES IX - PAGE; IMAGES V; IMAGES XV - Pachiderme; James Clark Ross; Joides Resolution; JOPSII-8; JR20110128; JR244; JR244-GC528; KAL; Kasten corer; KF13; KF16; KL; KM31; KN_USA; KN159-5; KN166-2; Knorr; KNR140; KNR140-2-51GGC; KNR140-51GGC; KNR159-5; KNR159-5-36GGC; KNR159-5-42JPC; KNR166-2; KNR166-2-26; KNR166-2-26JPC; KNR166-2-29; KNR166-2-29JPC; KNR166-2-31; KNR166-2-31JPC; KNR166-2-73; KNR166-2-73GGC; KNR197-10; KNR197-10-GGC17; KNR31GPC5; last 40 ky; LATITUDE; Leg162; Leg165; Leg172; Leg175; Leg94; Le Noroit; Le Suroît; LONGITUDE; M12392-1; M16/2; M17/2; M20/2; M25; M34/4; M35/1; M35003-4; M37/1; M39/1; M39/1_08-3; M39008-3; M42/4b; M46/2; M53; M53_169; M53/1; M6/6; M65/1; Marge Ibérique; Maria S. Merian; Marion Dufresne (1995); MD01-2461; MD022575; MD02-2575; MD02-2588; MD02-2588Q; MD02-2592; MD02-2594; MD03-2697; MD03-2698; MD03-2705; MD03-2707; MD04-2805CQ; MD04-2805Q; MD04-2845; MD07-3076; MD07-3076Q; MD08-3167; MD08-3180; MD08-3227G; MD09-3246; MD09-3256; MD09-3256Q; MD101; MD114; MD123; MD127; MD128; MD134; MD140; MD141; MD159; MD16-3511; MD16-3511Q; MD168; MD173; MD952002; MD95-2002; MD952006; MD95-2006; MD952010; MD95-2010; MD952014; MD95-2014; MD952037; MD95-2037; MD952039; MD95-2039; MD952040; MD95-2040; MD952041; MD95-2041; MD952042; MD95-2042; MD99-2281; MD99-2284; MD99-2331; MD99-2334; Meriadzec; Meteor (1964); Meteor (1986); Method comment; MSM20/3; N. Shetland channel; NA87-22; Namibia continental slope; Newfoundland margin; North Atlantic; North Atlantic/FLANK; North East Atlantic; Northeast Brasilian Margin; Norwegian Sea; OCE205-103GGC; OCE205-2-100GGC; OCE205-2-100GGGC; OCE205-2-103GGC; OCE326-GGC5; off Rio Paraiba do Sul; off West Africa; PALEOCINAT; PALEOCINAT II; PC; Persistent Identifier; PICABIA; Piston corer; Piston corer (BGR type); Polarstern; Porto Seamount; PRIVILEGE; PS2644-5; PS31; PS31/160-5; RAPiD-10-1P; RAPiD-17-5P; Reference/source; RETRO-2; REYKJANES-RÜCKEN; S94-2-KS04; SL; SO82; SO82_5-2; Sonne; South Atlantic; South Atlantic Ocean; Southern Ocean; South of Iceland; SU81-18; SU90-08; SU90-24; SU92; SU92-03; SWAF; Tagus-Sado canyon system; TNO57-21; Uniform resource locator/link to graphic; V29; V29-202; Vema; Victor Hensen; Vigo; Voring Plateau; western South Atlantic
    Materialart: Dataset
    Format: text/tab-separated-values, 563 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 9
    Publikationsdatum: 2024-06-18
    Beschreibung: Der Bereich des Meßtischblattes 6311 Lauterecken im Saar-Nahe-Gebiet (SW-Deutschland) wurde anhand einer geologischen, ingenieurgeologischen, hydrogeologischen und morphologischen Untersuchung einer Stabilitätsanalyse der Hänge und Böschungen unterzogen, die durch die Verwertung klimatologischer Daten vervollständigt wurde. Das Ergebnis liegt in einer Stabilitätskarte sowie in einer Analyse der gesammelten Daten vor. Soweit die Untersuchung des Modellgebietes von ca. 130 km21 Größe (etwa 5% der Fläche des Saar-Nahe-Gebietes) eine Antwort zuläßt, sind Hänge und Böschungen im sedimentären Rotliegenden des Saar-Nahe-Gebietes bereits ab 7° Hangneigung potentiell rutschgefährdet. Das rutschgefährdete Areal umfaßt etwa 10% der untersuchten Fläche. Ca. 2,6% wurden von Massenbewegungen betroffen. Kriechen und Gleiten sind die häufigsten Arten der Massenbewegungen. Die beteiligten stratigraphischen Einheiten sind neben den Deckschichten die Quirnbacher, Jeckenbacher und Lautereckener Schichten des Unteren Rotliegenden. Künstliche Böschungs-, An- und Einschnitte in den für das Unterrotliegende charakteristischen Wechsellagerungen von Ton-, Schluff- und Sandsteinen, stellen ein permanentes Stabilitätsproblem dar.
    Beschreibung: Abstract: This report deals with the analysis of stability of slopes which occur on the map of Lauterecken, Saar-Nahe-area, SW-Germany. A geological, engineering geological, hydrogeological and morphological study was made, additionally, climatological data were taken into account; the results of it are analyzed and plotted in a stability map. Conclusions: Taking the regarded territory of approximately 130 km2 (about 5% of the area of the Saar-Nahe-area), it can be stated that slopes in the Saar-Nahe-area are potential landslide areas, if the inclination of the slopes is 7° or more. Within an area of 10% landslides are probable to take place. Within 2,6% mass movements happened or are going on. Creep and sliding are the most abundant forms of mass movements. Slope instability occours preferentially in weathered rocks, Quirnbach beds, Jeckenbach beds and Lauterecken beds of the Lower Permian. Steep roadcuts occurring in alternating sandstone and siltstone beds are very likely to cause stability problems.
    Beschreibung: research
    Schlagwort(e): ddc:550 ; Rutschungen ; Saar-Nahe-Becken ; TK 6311 ; Rotliegend
    Sprache: Deutsch
    Materialart: doc-type:article , publishedVersion
    Standort Signatur Erwartet Verfügbarkeit
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  • 10
    Publikationsdatum: 2024-06-18
    Beschreibung: In verschiedenen Hanglagen der Ortsgemeinde Essenheim in Rheinhessen (Rheinland-Pfalz) ist der Untergrund rutschgefährdet oder es sind fossile Rutschungen vorhanden. In einer dieser Hanglagen wurde die Erweiterung des Baugebietes „Domherrngärten" geplant. In der Folge dessen war zu klären, unter welchen Randbedingungen die Bebauung realisiert werden kann. Hierzu wurden in mehreren Kampagnen der geologische Untergrund mit Kernbohrungen untersucht und Inklinometermessstellen zur Beobachtung von Hangbewegungen eingerichtet. Die Untersuchungsergebnisse wurden im Rahmen einer Bachelorarbeit zur Durchführung von Standsicherheitsberechnungen genutzt. Auf der Basis aller Untersuchungsergebnisse werden Vorsorgemaßnahmen für die Bebauung in einem rutschgefährdetem Hang aufgezeigt.
    Beschreibung: Abstract: Various slopes in the village Essenheim in Rhinehessen/ Rhineland-Pala- tinate are prone to landslides. The planed extension of the building area „Domherrngärten II" is part of such an area. In succession it had to be discussed under which circumstances construction is possible. To analyze the geological features core drillings with rock sampling were executed as well as inclinometers (measurements to detect motion of the slope). The taken data was used in a Bachelor thesis to evaluate the slope stability. On the base of all results references for building on instable slopes are given.
    Beschreibung: research
    Schlagwort(e): ddc:624.151 ; Mainzer Becken ; Rutschungen ; Ingenieurgeologie ; TK 6014
    Sprache: Deutsch
    Materialart: doc-type:article , publishedVersion
    Standort Signatur Erwartet Verfügbarkeit
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