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 inJournal of earth science (Wuhan, China) Vol. 24; no. 4; pp. 569 - 578
Main Author 李清洋 潘保田 胡小飞 胡振波 李富强 杨顺智
Format Journal Article
LanguageEnglish
Published Berlin/Heidelberg Springer Berlin Heidelberg 01.08.2013
Springer Nature B.V
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ISSN1674-487X
1867-111X
DOI10.1007/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.
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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Keywords North Qilian Mountain
fault activity
AFT
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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.
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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...
SourceID proquest
crossref
springer
chongqing
SourceType Aggregation Database
Enrichment Source
Index Database
Publisher
StartPage 569
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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https://link.springer.com/article/10.1007/s12583-013-0350-1
https://www.proquest.com/docview/1437177174
https://www.proquest.com/docview/1448713340
https://www.proquest.com/docview/1671474135
Volume 24
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