Collision Event during 177-135 Ma on the Eastern Margin of the Qinghai-Tibet Plateau: Evidence from 40Ar/ 39Ar Dating for Basalts on the Western Margin of the Yangtze Platform

Geochronology of continental flood basalts sampled from the Emei large igneous province (LIP) on the western margin of the Yangtze platform was investigated by the laser microprobe 40Ar/39Ar dating technique. These basalts yield a fairly wide range of 40Ar/39Ar ages, varying from 259 to 135 Ma. One...

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Published inActa geologica Sinica (Beijing) Vol. 76; no. 2; pp. 194 - 204
Main Authors Zengqian, HOU, Wen, CHEN, Jiren, LU
Format Journal Article
LanguageEnglish
Published Oxford, UK Blackwell Publishing Ltd 01.06.2002
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Online AccessGet full text
ISSN1000-9515
1755-6724
DOI10.1111/j.1755-6724.2002.tb00085.x

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Abstract Geochronology of continental flood basalts sampled from the Emei large igneous province (LIP) on the western margin of the Yangtze platform was investigated by the laser microprobe 40Ar/39Ar dating technique. These basalts yield a fairly wide range of 40Ar/39Ar ages, varying from 259 to 135 Ma. One basalt sample, at least altered, recorded the oldest 40Ar/39Ar age of about 259 Ma, corresponding to a peak eruption age of the Emei LIP continental flood basalts. Most of the samples yield much younger ages from 135 to 177 Ma, which are consistent with the K-Ar ages for the same samples (122.8-172.1 Ma). The dating data suggest that these Permian basalts had been widely affected by the regional tectonothermal event at 177-135 Ma. The event was probably caused by the convergence and collision among the Laurasia, Yangtze and Qiangtang-Qamdo continental blocks on the eastern margin of the Qinghai-Tibet plateau after the late Triassic. The age of the event reflects the timing of the peak collisional orogeny.
AbstractList Geochronology of continental flood basalts sampled from the Emei large igneous province (LIP) on the western margin of the Yangtze platform was investigated by the laser microprobe 40Ar/39Ar dating technique. These basalts yield a fairly wide range of 40Ar/39Ar ages, varying from 259 to 135 Ma. One basalt sample, at least altered, recorded the oldest 40Ar/39Ar age of about 259 Ma, corresponding to a peak eruption age of the Emei LIP continental flood basalts. Most of the samples yield much younger ages from 135 to 177 Ma, which are consistent with the K‐Ar ages for the same samples (122.8–172.1 Ma). The dating data suggest that these Permian basalts had been widely affected by the regional tectonothermal event at 177–135 Ma. The event was probably caused by the convergence and collision among the Laurasia, Yangtze and Qiangtang‐Qamdo continental blocks on the eastern margin of the Qinghai‐Tibet plateau after the late Triassic. The age of the event reflects the timing of the peak collisional orogeny.
Author Zengqian, HOU
Jiren, LU
Wen, CHEN
AuthorAffiliation Institute of Mineral Resources, Chinese Academy of Geological Sciences Beijing, 100037 Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037;3College of Earth Sciences, China University of Geosciences, Beijing 100029 Institute of Mineral Resources, Chinese Academy of Geological Sciences Beijing, 100037
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Born in June, 1961; graduated from the specialty of geology, Hebei College of Geology in 1982. He got his master's degree and Ph.D. at China University of Geosciences in 1985 and 1988, respectively. His main interests include volcanism, submarine thermal waters and related metallogenesis. He has made marked achievements in his research and published a number of monographs and dozens of scientific papers.
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Snippet Geochronology of continental flood basalts sampled from the Emei large igneous province (LIP) on the western margin of the Yangtze platform was investigated by...
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istex
chongqing
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StartPage 194
SubjectTerms 40Ar/39Ar
40Ar/39Ar age
age
basalts
basalts in the Emei LIP
collisional
collisional orogeny
Emei
LIP
orogeny
plateau
Qinghai-Tibet
Qinghai-Tibet plateau
the
Title Collision Event during 177-135 Ma on the Eastern Margin of the Qinghai-Tibet Plateau: Evidence from 40Ar/ 39Ar Dating for Basalts on the Western Margin of the Yangtze Platform
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