中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Fission-track evidence of tectonic evolution in the northwestern Qaidam Basin, China

文献类型:期刊论文

作者Sun, Guo-Qiang1; Liu, Wei-Ming1,2; Guo, Jia-Jia1,2; Wang, Ye-Tong1,2
刊名JOURNAL OF EARTH SYSTEM SCIENCE
出版日期2018-02-01
卷号127期号:1
关键词Apatite Fission-track Zircon Fission-track Tectonic Evolution Qaidam Basin
ISSN号0253-4126
DOI10.1007/s12040-017-0914-z
文献子类Article
英文摘要Fission-track dating was conducted on zircons and apatites from 11 cores of the upper Xiaganchaigou Formation and lower Shangganchaigou Formation (northwestern Qaidam Basin). The obtained apatite fission-track age is 3.1-61.9 Ma, and the zircon fission-track age is 49.2-123.5 Ma. Although the average apatite age is consistent with ages predicted from the stratigraphy, nine of the 11 apatite fission-track ages have P(chi(2)) < 5%, indicating that the grains experienced heterogeneous annealing after sedimentation. The average zircon age is greater than that indicated by stratigraphy, and all eight zircon fission ages have P(chi(2)) > 5%, exhibiting consistent characteristics and indicating that zircons retain provenance age information after burial. From the zircon and apatite ages, the fission-track length distribution, and the geological setting, the northwestern Qaidam Basin has experienced two tectonothermal events since the Late Mesozoic, at 39.1 +/- 9.3 to 133.7 +/- 6.6 Ma and 1.2 +/- 0.6 to 32.0 +/- 3.0 Ma. The earlier (39.1-133.7 Ma) tectonothermal event resulted from the initial collision of the Indian and Eurasian plates. As a consequence of the collision, the Altyn Tagh fault, which forms the northwestern boundary of the Qaidam Basin, began to develop. Subsequently, uplift of the Altyn Tagh mountains began and the northwestern depression of the Qaidam Basin started to form. The later (1.2-32.0 Ma) tectonothermal event resulted from further collision of the Indian and Eurasian plates along the Yarlung Tsangpo suture zone. Strata in the Qaidam Basin were further deformed by transpression in this period and this period played a crucial role in petroleum accumulation.
WOS关键词ALTYN-TAGH FAULT ; NW CHINA ; THERMAL HISTORY ; CONSTRAINTS ; APATITE ; HIMALAYA ; INDIA ; THERMOCHRONOLOGY ; KUMAON ; TEMPERATURE
WOS研究方向Geology ; Science & Technology - Other Topics
语种英语
WOS记录号WOS:000426596600012
出版者INDIAN ACAD SCIENCES
资助机构'Western Light' Talents Training Program of CAS ; 'Western Light' Talents Training Program of CAS ; Nature Science Foundation of Gansu Province(1308RJZA310) ; Nature Science Foundation of Gansu Province(1308RJZA310) ; Key Laboratory Project of Gansu Province(1309RTSA041) ; Key Laboratory Project of Gansu Province(1309RTSA041) ; 'Western Light' Talents Training Program of CAS ; 'Western Light' Talents Training Program of CAS ; Nature Science Foundation of Gansu Province(1308RJZA310) ; Nature Science Foundation of Gansu Province(1308RJZA310) ; Key Laboratory Project of Gansu Province(1309RTSA041) ; Key Laboratory Project of Gansu Province(1309RTSA041) ; 'Western Light' Talents Training Program of CAS ; 'Western Light' Talents Training Program of CAS ; Nature Science Foundation of Gansu Province(1308RJZA310) ; Nature Science Foundation of Gansu Province(1308RJZA310) ; Key Laboratory Project of Gansu Province(1309RTSA041) ; Key Laboratory Project of Gansu Province(1309RTSA041) ; 'Western Light' Talents Training Program of CAS ; 'Western Light' Talents Training Program of CAS ; Nature Science Foundation of Gansu Province(1308RJZA310) ; Nature Science Foundation of Gansu Province(1308RJZA310) ; Key Laboratory Project of Gansu Province(1309RTSA041) ; Key Laboratory Project of Gansu Province(1309RTSA041)
源URL[http://ir.iggcas.ac.cn/handle/132A11/93132]  
专题地质与地球物理研究所_兰州油气中心
通讯作者Sun, Guo-Qiang
作者单位1.Chinese Acad Sci, Key Lab Petr Resources, Gansu Prov Key Lab Petr Resources Res, Inst Geol & Geophys, Lanzhou 730000, Gansu, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
推荐引用方式
GB/T 7714
Sun, Guo-Qiang,Liu, Wei-Ming,Guo, Jia-Jia,et al. Fission-track evidence of tectonic evolution in the northwestern Qaidam Basin, China[J]. JOURNAL OF EARTH SYSTEM SCIENCE,2018,127(1).
APA Sun, Guo-Qiang,Liu, Wei-Ming,Guo, Jia-Jia,&Wang, Ye-Tong.(2018).Fission-track evidence of tectonic evolution in the northwestern Qaidam Basin, China.JOURNAL OF EARTH SYSTEM SCIENCE,127(1).
MLA Sun, Guo-Qiang,et al."Fission-track evidence of tectonic evolution in the northwestern Qaidam Basin, China".JOURNAL OF EARTH SYSTEM SCIENCE 127.1(2018).

入库方式: OAI收割

来源:地质与地球物理研究所

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