Apatite Fission Track Constraints on the Pattern of Faulting in the North Qilian Mountain
The Qilian (祁连) Mountain is an active orogenic belt located at the northeastern margin of the Tibetan Plateau. During the process of continuous convergence between Indian and Eurasian plates, the Qilian Mountain grow correspondingly by means of reaction of old faults and generation of new ones. Here...
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Published in | Journal of earth science (Wuhan, China) Vol. 24; no. 4; pp. 569 - 578 |
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Main Author | |
Format | Journal Article |
Language | English |
Published |
Berlin/Heidelberg
Springer Berlin Heidelberg
01.08.2013
Springer Nature B.V |
Subjects | |
Online Access | Get full text |
ISSN | 1674-487X 1867-111X |
DOI | 10.1007/s12583-013-0350-1 |
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Abstract | The Qilian (祁连) Mountain is an active orogenic belt located at the northeastern margin of the Tibetan Plateau. During the process of continuous convergence between Indian and Eurasian plates, the Qilian Mountain grow correspondingly by means of reaction of old faults and generation of new ones. Here we present apatite fission-track data along a river profile crossing three minor fault (the Minle (民乐)-Damaying (大马营) fault, the Huangcheng (皇城)-Taerzhuang (塔尔庄) fault and the Kangningqiao (唐宁桥) fault) which compose the North Qilian fault (NQF) to test the timing and pat- terns of the fault activities. Apatite fission-track (AFT) results indicate that these minor faults expe- rienced two active phases in the Cretaceous and the Oligocene-Miocene. Further research indicate that the initiation timing of faulting became younger northward in both active periods and the later phase probably more active than the former phase. These tectonic activities might be highly related to the docking of the Lhasa Block to the south in the Cretaceous and uplift and expansion of the Tibetan Pla- teau in the Cenozoic. |
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AbstractList | The Qilian (è¿z) Mountain is an active orogenic belt located at the northeastern margin of the Tibetan Plateau. During the process of continuous convergence between Indian and Eurasian plates, the Qilian Mountain grow correspondingly by means of reaction of old faults and generation of new ones. Here we present apatite fission-track data along a river profile crossing three minor fault (the Minle ()-Damaying () fault, the Huangcheng ()-Taerzhuang () fault and the Kangningqiao () fault) which compose the North Qilian fault (NQF) to test the timing and patterns of the fault activities. Apatite fission-track (AFT) results indicate that these minor faults experienced two active phases in the Cretaceous and the Oligocene-Miocene. Further research indicate that the initiation timing of faulting became younger northward in both active periods and the later phase probably more active than the former phase. These tectonic activities might be highly related to the docking of the Lhasa Block to the south in the Cretaceous and uplift and expansion of the Tibetan Plateau in the Cenozoic.[PUBLICATION ABSTRACT] The Qilian (祁连) Mountain is an active orogenic belt located at the northeastern margin of the Tibetan Plateau. During the process of continuous convergence between Indian and Eurasian plates, the Qilian Mountain grow correspondingly by means of reaction of old faults and generation of new ones. Here we present apatite fission-track data along a river profile crossing three minor fault (the Minle (民乐)-Damaying (大马营) fault, the Huangcheng (皇城)-Taerzhuang (塔尔庄) fault and the Kangningqiao (唐宁桥) fault) which compose the North Qilian fault (NQF) to test the timing and pat- terns of the fault activities. Apatite fission-track (AFT) results indicate that these minor faults expe- rienced two active phases in the Cretaceous and the Oligocene-Miocene. Further research indicate that the initiation timing of faulting became younger northward in both active periods and the later phase probably more active than the former phase. These tectonic activities might be highly related to the docking of the Lhasa Block to the south in the Cretaceous and uplift and expansion of the Tibetan Pla- teau in the Cenozoic. The Qilian ([Chinese characters]) Mountain is an active orogenic belt located at the northeastern margin of the Tibetan Plateau. During the process of continuous convergence between Indian and Eurasian plates, the Qilian Mountain grow correspondingly by means of reaction of old faults and generation of new ones. Here we present apatite fission-track data along a river profile crossing three minor fault (the Minle (ae super(1))-Damaying ([Chinese characters]) fault, the Huangcheng ([Chinese characters])-Taerzhuang ([Chinese characters]) fault and the Kangningqiao ([Chinese characters]) fault) which compose the North Qilian fault (NQF) to test the timing and patterns of the fault activities. Apatite fission-track (AFT) results indicate that these minor faults experienced two active phases in the Cretaceous and the Oligocene-Miocene. Further research indicate that the initiation timing of faulting became younger northward in both active periods and the later phase probably more active than the former phase. These tectonic activities might be highly related to the docking of the Lhasa Block to the south in the Cretaceous and uplift and expansion of the Tibetan Plateau in the Cenozoic. The Qilian (祁连) Mountain is an active orogenic belt located at the northeastern margin of the Tibetan Plateau. During the process of continuous convergence between Indian and Eurasian plates, the Qilian Mountain grow correspondingly by means of reaction of old faults and generation of new ones. Here we present apatite fission-track data along a river profile crossing three minor fault (the Minle (民乐)-Damaying (大马营) fault, the Huangcheng (皇城)-Taerzhuang (塔尔庄) fault and the Kangningqiao (康宁桥) fault) which compose the North Qilian fault (NQF) to test the timing and patterns of the fault activities. Apatite fission-track (AFT) results indicate that these minor faults experienced two active phases in the Cretaceous and the Oligocene-Miocene. Further research indicate that the initiation timing of faulting became younger northward in both active periods and the later phase probably more active than the former phase. These tectonic activities might be highly related to the docking of the Lhasa Block to the south in the Cretaceous and uplift and expansion of the Tibetan Plateau in the Cenozoic. |
Author | 李清洋 潘保田 胡小飞 胡振波 李富强 杨顺智 |
AuthorAffiliation | Key Laboratory of Western China' s Environmental Systems (Ministry of Education), Research School of Arid Environment & Climate Change, Lanzhou University, Lanzhou 730000, China Sulige Gasfield Development Company, PCOC, Xi' an 710018, China |
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Notes | Qingyang Li*, Baotian Pan , Xiaofei Hu, Zhenbo Hu , Fuqiang Li Key Laboratory of Western China' s Environmental Systems (Ministry of Education), Research School of Arid Environment & Climate Change, Lanzhou University, Lanzhou 730000, China Shunzhi Yang Sulige Gasfield Development Company, PCOC, Xi' an 710018, China The Qilian (祁连) Mountain is an active orogenic belt located at the northeastern margin of the Tibetan Plateau. During the process of continuous convergence between Indian and Eurasian plates, the Qilian Mountain grow correspondingly by means of reaction of old faults and generation of new ones. Here we present apatite fission-track data along a river profile crossing three minor fault (the Minle (民乐)-Damaying (大马营) fault, the Huangcheng (皇城)-Taerzhuang (塔尔庄) fault and the Kangningqiao (唐宁桥) fault) which compose the North Qilian fault (NQF) to test the timing and pat- terns of the fault activities. Apatite fission-track (AFT) results indicate that these minor faults expe- rienced two active phases in the Cretaceous and the Oligocene-Miocene. Further research indicate that the initiation timing of faulting became younger northward in both active periods and the later phase probably more active than the former phase. These tectonic activities might be highly related to the docking of the Lhasa Block to the south in the Cretaceous and uplift and expansion of the Tibetan Pla- teau in the Cenozoic. North Qilian Mountain, AFT, fault activity. 42-1788/P SourceType-Scholarly Journals-1 ObjectType-Feature-1 content type line 14 ObjectType-Article-1 ObjectType-Feature-2 content type line 23 |
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Snippet | The Qilian (祁连) Mountain is an active orogenic belt located at the northeastern margin of the Tibetan Plateau. During the process of continuous convergence... The Qilian (祁连) Mountain is an active orogenic belt located at the northeastern margin of the Tibetan Plateau. During the process of continuous convergence... The Qilian (è¿z) Mountain is an active orogenic belt located at the northeastern margin of the Tibetan Plateau. During the process of continuous convergence... The Qilian ([Chinese characters]) Mountain is an active orogenic belt located at the northeastern margin of the Tibetan Plateau. During the process of... |
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SubjectTerms | Apatite Belts Biogeosciences Blocking Cenozoic Convergence Cretaceous Earth and Environmental Science Earth science Earth Sciences Fault diagnosis Faults Geochemistry Geology Geotechnical Engineering & Applied Earth Sciences Minerals Miocene Mountains Oligocene Phases Time measurements 北祁连山 印度板块 拉萨地块 断层活动 欧亚板块 磷灰石裂变径迹 约束模式 青藏高原 |
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Title | Apatite Fission Track Constraints on the Pattern of Faulting in the North Qilian Mountain |
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