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  • 1
    Call number: M 18.91817
    Description / Table of Contents: This book is focused on the basics of applying thermochronology to geological and tectonic problems, with the emphasis on fission-track thermochronology. It is conceived for relatively new practitioners to thermochronology, as well as scientists experienced in the various methods. The book is structured in two parts. Part I is devoted to the fundamentals of the fission-track method, to its integration with other geochronologic methods, and to the basic principles of statistics for fission-track dating and sedimentology applied to detrital thermochronology. Part I also includes the historical development of the technique and thoughts on future directions. Part II is devoted to the geological interpretation of the thermochronologic record. The thermal frame of reference and the different approaches for the interpretation of fission-track data within a geological framework of both basement and detrital studies are discussed in detail. Separate chapters demonstrate the application of fission-track thermochronology from various perspectives (e.g., tectonics, petrology, stratigraphy, hydrocarbon exploration, geomorphology), with other chapters on the application to basement rocks in orogens, passive continental margins and cratonic interiors, as well as various applications of detrital thermochronology.
    Type of Medium: Monograph available for loan
    Pages: XV, 393 Seiten , Illustrationen
    ISBN: 9783319894195
    Series Statement: Springer Textbooks in Earth Sciences, Geography and Environment
    Classification:
    Applied Geology
    Language: English
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  • 2
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    PANGAEA
    In:  Supplement to: Fitzgerald, Paul G (2001): Apatite fission track ages associated with the altered igneous intrusive in beacon sandstone near the base of CRP-3, Victoria Land Basin, Antarctica. Terra Antartica, 8(4), 585-592, hdl:10013/epic.28218.d001
    Publication Date: 2023-06-27
    Description: The Cape Roberts drillhole 3 (CRP-3) on the western edge of the Victoria Land Basin, Antarctica cored through a highly altered igneous intrusion intruded into Paleozoic sedimentary basement. This intrusion was regarded as highly enigmatic as its origin could represent volcanism associated with early rifling of the Victoria Land Basin, later renewed rifting within the Terror rift, or Jurassic tholeiitic magmatism. Direct methods to date the intrusion by U-Pb dating of zircon or fission track analysis failed due to insufficient quantities of these minerals. Apatite fission track (AFT) analysis on the adjacent sedimentary basement, the Devonian Beacon Supergroup sandstone, yielded an age of 101 ± 6 Ma and a mean track length of 12.3 µm with a 1.9 µm standard deviation. The fission tracks were not annealed in the Cenozoic and thus the intrusion must be older than this. This observation, plus race element chemistry of the intrusion suggest it is most likely the same age and original composition as the middle Jurassic sills and dykes of the Transantarctic Mountains. The AFT age is similar to the onshore regional AFT stratigraphy and reflects complete thermal overprinting in the Jurassic, residence in an apatite partial annealing zone, followed by exhumation in the early Cenozoic and down-faulting at least 3 km to its present position. However, the sample of Beacon sandstone has an AFT age 'too young' and a confined track length distribution 'too short' relative to the results a sample from an onland equivalent stratigraphic position should yield in the simplest scenario. This is possibly due to the position of the CRP-3 basement on the western edge of the West Antarctic rift system, where it underwent periods of rifting and elevated thermal gradients in the Jurassic, Cretaceous, Eocene and Oligocene causing annealing of the sample. Alternatively, this sample reflects a more complex thermal history involving Cretaceous as well as Cenozoic denudation, prior to being down faulted to its present position.
    Keywords: Age, dated; Age, dated standard deviation; Cape Roberts Project; Core wireline system; CRP; CRP-3; CWS; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Error, relative; Grains, counted/analyzed; Length; Lithology/composition/facies; Probability, chi-square test; Ross Sea; Sample comment; Sampling/drilling from ice; Standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 13 data points
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  • 3
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    PANGAEA
    In:  Supplement to: Monteleone, Brian D; Baldwin, Suzanne L; Ireland, Trevor R; Fitzgerald, Paul G (2001): Thermochronologic constraints for the tectonic evolution of the Moresby Seamount, Woodlark Basin, Papua New Guinea. In: Huchon, P; Taylor, B; Klaus, A (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 180, 1-35, https://doi.org/10.2973/odp.proc.sr.180.173.2001
    Publication Date: 2024-01-09
    Description: During Ocean Drilling Program (ODP) Leg 180, 11 sites were drilled in the vicinity of the Moresby Seamount to study processes associated with the transition from continental rifting to seafloor spreading in the Woodlark Basin. This paper presents thermochronologic (40Ar/39Ar, 238U/206Pb, and fission track) results from igneous rocks recovered during ODP Leg 180 that help constrain the latest Cretaceous to present-day tectonic development of the Woodlark Basin. Igneous rocks recovered (primarily from Sites 1109, 1114, 1117, and 1118) consist of predominantly diabase and metadiabase, with minor basalt and gabbro. Zircon ion microprobe analyses gave a 238U/206Pb age of 66.4 ± 1.5 Ma, interpreted to date crystallization of the diabase. 40Ar/39Ar plagioclase apparent ages vary considerably according to the degree to which the diabase was altered subsequent to crystallization. The least altered sample (from Site 1109) yielded a plagioclase isochron age of 58.9 ± 5.8 Ma, interpreted to represent cooling following intrusion. The most altered sample (from Site 1117) yielded an isochron age of 31.0 ± 0.9 Ma, interpreted to represent a maximum age for the timing of subsequent hydrothermal alteration. The diabase has not been thermally affected by Miocene-Pliocene rift-related events, supporting our inference that these rocks have remained at shallow and cool levels in the crust (i.e., upper plate) since they were partially reset as a result of middle Oligocene hydrothermal alteration. These results suggest that crustal extension in the vicinity of the Moresby Seamount, immediately west of the active seafloor spreading tip, is being accommodated by normal faulting within latest Cretaceous to early Paleocene oceanic crust. Felsic clasts provide additional evidence for middle Miocene and Pliocene magmatic events in the region. Two rhyolitic clasts (from Sites 1110 and 1111) gave zircon 238U/206Pb ages of 15.7 ± 0.4 Ma and provide evidence for Miocene volcanism in the region. 40Ar/39Ar total fusion ages on single grains of K-feldspar from these clasts yielded younger apparent ages of 12.5 ± 0.2 and 14.4 ± 0.6 Ma due to variable sericitization of K-feldspar phenocrysts. 238U/206Pb zircon, 40Ar/39Ar K-feldspar and biotite total fusion, and apatite fission track analysis of a microgranite clast (from Site 1108) provide evidence for the existence of a rapidly cooled 3.0 to 1.8 Ma granitic protolith. The clast may have been transported longitudinally from the west (e.g., from the D'Entrecasteaux Islands). Alternatively, it may have been derived from a more proximal, but presently unknown, source in the vicinity of the Moresby Seamount.
    Keywords: Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 4
    Publication Date: 2024-01-09
    Keywords: 180-1108B; 180-1109D; 180-1110B; 180-1111A; 180-1117A; 180-1118A; Age, dated; Age, dated standard deviation; DRILL; Drilling/drill rig; Elevation of event; Event label; Joides Resolution; Latitude of event; Leg180; Longitude of event; Method comment; Minerals; Ocean Drilling Program; ODP; Rock type; Sample code/label; Sample comment; Solomon Sea
    Type: Dataset
    Format: text/tab-separated-values, 140 data points
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  • 5
    Publication Date: 2024-01-09
    Keywords: 180-1108B; 180-1109D; 180-1110B; 180-1111A; 180-1117; 180-1117A; 180-1118A; Age, 40Ar/39Ar Argon-Argon; Age, dated; Age, dated standard deviation; Argon-36/Argon-39; Argon-37/Argon-39; Argon-39; Argon-40; Argon-40/Argon-39; COMPCORE; Composite Core; DRILL; Drilling/drill rig; Elevation of event; Event label; Grain size description; Joides Resolution; Latitude of event; Leg180; Longitude of event; Method comment; Minerals; Ocean Drilling Program; ODP; Parameter; Sample code/label; Sample mass; Solomon Sea; Temperature, technical
    Type: Dataset
    Format: text/tab-separated-values, 1266 data points
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  • 6
    Publication Date: 2024-01-09
    Keywords: 180-1108; 180-1110; 180-1111; 180-1117A; Age, dated; Age, dated standard deviation; Age, Uranium-Lead; COMPCORE; Composite Core; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Joides Resolution; Latitude of event; Lead-204/Lead-206, error; Lead-204/Lead-206 ratio; Lead-207/Lead-206, standard error; Lead-207/Lead-206 ratio; Leg180; Longitude of event; Ocean Drilling Program; ODP; Rock type; Sample code/label; Sample ID; Solomon Sea; Thorium; Thorium/Uranium ratio; Uranium; Uranium-238/Lead-206, standard error; Uranium-238/Lead-206 ratio
    Type: Dataset
    Format: text/tab-separated-values, 332 data points
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  • 7
    Publication Date: 2019-10-17
    Description: Since the first discovery of ultrahigh pressure (UHP) rocks 30 years ago in the Western Alps, the mechanisms for exhumation of (U)HP terranes worldwide are still debated. In the western Mediterranean, the presently accepted model of synconvergent exhumation (e.g., the channel-flow model) is in conflict with parts of the geologic record. We synthesize regional geologic data and present alternative exhumation mechanisms that consider the role of divergence within subduction zones. These mechanisms, i.e., (i) the motion of the upper plate away from the trench and (ii) the rollback of the lower plate, are discussed in detail with particular reference to the Cenozoic Adria-Europe plate boundary, and along three different transects (Western Alps, Calabria-Sardinia, and Corsica-Northern Apennines). In the Western Alps, (U)HP rocks were exhumed from the greatest depth at the rear of the accretionary wedge during motion of the upper plate away from the trench. Exhumation was extremely fast, and associated with very low geothermal gradients. In Calabria, HP rocks were exhumed from shallower depths and at lower rates during rollback of the Adriatic plate, with repeated exhumation pulses progressively younging toward the foreland. Both mechanisms were active to create boundary divergence along the Corsica-Northern Apennines transect, where European southeastward subduction was progressively replaced along strike by Adriatic northwestward subduction. The tectonic scenario depicted for the Western Alps trench during Eocene exhumation of (U)HP rocks correlates well with present-day eastern Papua New Guinea, which is presented as a modern analog of the Paleogene Adria-Europe plate boundary.
    Description: Published
    Description: 1786–1824
    Description: 1T. Struttura della Terra
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 8
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] As lithospheric plates are subducted, rocks are metamorphosed under high-pressure and ultrahigh-pressure conditions to produce eclogites and eclogite facies metamorphic rocks. Because chemical equilibrium is rarely fully achieved, eclogites may preserve in their distinctive mineral assemblages and ...
    Type of Medium: Electronic Resource
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  • 9
    Publication Date: 2007-04-26
    Print ISSN: 1085-9195
    Electronic ISSN: 1559-0283
    Topics: Biology , Medicine
    Published by Springer
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  • 10
    Publication Date: 2007-08-01
    Print ISSN: 0006-291X
    Electronic ISSN: 1090-2104
    Topics: Biology , Chemistry and Pharmacology , Physics
    Published by Elsevier
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