Tab. 1: Zircon isotopic data and rock ages from the Antarctic Peninsula ...
Morphological and U-Pb isotope studies on sedimentary zircons reflect the orogenic evolution of their former host rocks. The orogenic history of detrital zircons from the Trinity Peninsula Formation (TPF) defines the former geological surrounding of the sedimentation basin of the TPF. Same few weil...
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ftdatacite:10.1594/pangaea.755487 2024-09-15T17:47:22+00:00 Tab. 1: Zircon isotopic data and rock ages from the Antarctic Peninsula ... Miller, Hubert Loske, Werner Kramm, Ulrich 1987 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.755487 https://doi.pangaea.de/10.1594/PANGAEA.755487 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Event label Sample comment Size fraction Mass Lead-208/Lead-206 ratio Lead-207/Lead-206 ratio Lead-206/Lead-204 ratio Uranium Lead Lead-206 Lead-206/Uranium-238 ratio Lead-207/Uranium-235 ratio Age, dated Geological sample Measured Corrected Age, 238U/206Pb Uranium-Lead Age, 235U/207Pb Uranium-Lead Age, 206Pb/207Pb Lead-Lead dataset Supplementary Dataset Dataset 1987 ftdatacite https://doi.org/10.1594/pangaea.755487 2024-08-01T10:50:04Z Morphological and U-Pb isotope studies on sedimentary zircons reflect the orogenic evolution of their former host rocks. The orogenic history of detrital zircons from the Trinity Peninsula Formation (TPF) defines the former geological surrounding of the sedimentation basin of the TPF. Same few weil rounded, polycyclic zircons of Precambrian age and Cambrian overprint give hints for an old cratonic source rock. Because of their very low frequency compared with euhedral types, the contribution of an cratonic shield area to the bulk of the sedimentary debris is neglectable low. Euhedral zircons of granitoid origin and Carboniferous age indicate a derivation from an area of widespread Carboniferous intrusions. Except for southern South America and unsurveyed regions in the Antarctic Peninsula itself, no region could deliver zircons with a Carboniferous age record. The only acceptable explanation for the origin of these zircons is a position of the Antarctic Peninsula during the sedimentation of the TPF ... : s = S-type zircons, c = C-type zirkons, r = reddish colour, b = brownish color, p = pink colour, a = all colours, m = metamict. Usedconstants: STEIGER & JÄGER (1977). Common-Pb composition: STACEY & KREAMERS (1975). Euhedral zirkons 400 Ma, xenomorphic zircons 700 and 800 Ma. Composition of Pb-blank: 208/204, 207/204, 206/204: 37.5, 15.5, 17.72 ... Dataset Antarc* Antarctic Antarctic Peninsula DataCite |
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ftdatacite |
language |
English |
topic |
Event label Sample comment Size fraction Mass Lead-208/Lead-206 ratio Lead-207/Lead-206 ratio Lead-206/Lead-204 ratio Uranium Lead Lead-206 Lead-206/Uranium-238 ratio Lead-207/Uranium-235 ratio Age, dated Geological sample Measured Corrected Age, 238U/206Pb Uranium-Lead Age, 235U/207Pb Uranium-Lead Age, 206Pb/207Pb Lead-Lead |
spellingShingle |
Event label Sample comment Size fraction Mass Lead-208/Lead-206 ratio Lead-207/Lead-206 ratio Lead-206/Lead-204 ratio Uranium Lead Lead-206 Lead-206/Uranium-238 ratio Lead-207/Uranium-235 ratio Age, dated Geological sample Measured Corrected Age, 238U/206Pb Uranium-Lead Age, 235U/207Pb Uranium-Lead Age, 206Pb/207Pb Lead-Lead Miller, Hubert Loske, Werner Kramm, Ulrich Tab. 1: Zircon isotopic data and rock ages from the Antarctic Peninsula ... |
topic_facet |
Event label Sample comment Size fraction Mass Lead-208/Lead-206 ratio Lead-207/Lead-206 ratio Lead-206/Lead-204 ratio Uranium Lead Lead-206 Lead-206/Uranium-238 ratio Lead-207/Uranium-235 ratio Age, dated Geological sample Measured Corrected Age, 238U/206Pb Uranium-Lead Age, 235U/207Pb Uranium-Lead Age, 206Pb/207Pb Lead-Lead |
description |
Morphological and U-Pb isotope studies on sedimentary zircons reflect the orogenic evolution of their former host rocks. The orogenic history of detrital zircons from the Trinity Peninsula Formation (TPF) defines the former geological surrounding of the sedimentation basin of the TPF. Same few weil rounded, polycyclic zircons of Precambrian age and Cambrian overprint give hints for an old cratonic source rock. Because of their very low frequency compared with euhedral types, the contribution of an cratonic shield area to the bulk of the sedimentary debris is neglectable low. Euhedral zircons of granitoid origin and Carboniferous age indicate a derivation from an area of widespread Carboniferous intrusions. Except for southern South America and unsurveyed regions in the Antarctic Peninsula itself, no region could deliver zircons with a Carboniferous age record. The only acceptable explanation for the origin of these zircons is a position of the Antarctic Peninsula during the sedimentation of the TPF ... : s = S-type zircons, c = C-type zirkons, r = reddish colour, b = brownish color, p = pink colour, a = all colours, m = metamict. Usedconstants: STEIGER & JÄGER (1977). Common-Pb composition: STACEY & KREAMERS (1975). Euhedral zirkons 400 Ma, xenomorphic zircons 700 and 800 Ma. Composition of Pb-blank: 208/204, 207/204, 206/204: 37.5, 15.5, 17.72 ... |
format |
Dataset |
author |
Miller, Hubert Loske, Werner Kramm, Ulrich |
author_facet |
Miller, Hubert Loske, Werner Kramm, Ulrich |
author_sort |
Miller, Hubert |
title |
Tab. 1: Zircon isotopic data and rock ages from the Antarctic Peninsula ... |
title_short |
Tab. 1: Zircon isotopic data and rock ages from the Antarctic Peninsula ... |
title_full |
Tab. 1: Zircon isotopic data and rock ages from the Antarctic Peninsula ... |
title_fullStr |
Tab. 1: Zircon isotopic data and rock ages from the Antarctic Peninsula ... |
title_full_unstemmed |
Tab. 1: Zircon isotopic data and rock ages from the Antarctic Peninsula ... |
title_sort |
tab. 1: zircon isotopic data and rock ages from the antarctic peninsula ... |
publisher |
PANGAEA |
publishDate |
1987 |
url |
https://dx.doi.org/10.1594/pangaea.755487 https://doi.pangaea.de/10.1594/PANGAEA.755487 |
genre |
Antarc* Antarctic Antarctic Peninsula |
genre_facet |
Antarc* Antarctic Antarctic Peninsula |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.755487 |
_version_ |
1810496570128334848 |