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Detrital Zircon Provenance of the Cenozoic Sequence, Kotli, Northwestern Himalaya, Pakistan; Implications for India-Asia Collision

文献类型：期刊论文

作者Awais, Muhammad2,8; Qasim, Muhammad1,4,5,6,7,8; Tanoli, Javed Iqbal1,5; Ding, Lin4,6,7,8; Sattar, Maryam9; Baig, Mirza Shahid3; Pervaiz, Shahab3
刊名MINERALS
出版日期2021-12-01
卷号11期号:12页码:15
关键词detrital zircon provenance Cenozoic sequence Hazara-Kashmir syntaxis Kashmir foreland-fold belt northwestern Himalaya India-Asia collision
DOI10.3390/min11121399
英文摘要This study reported the detrital zircon U-Pb geochronology of the Cenozoic sequence exposed in Kotli, northwestern Himalaya, Pakistan, which forms part of the Kashmir foreland basin. The U-Pb detrital age patterns of the Paleocene Patala Formation show a major age cluster between ~130-290 Ma, ~500-1000 Ma and ~1000-1500 Ma, which mainly resembles the lesser and higher Himalayan sequence. However, the younger age pattern (~130-290 Ma) can be matched to the ages of the ophiolites exposed along the Indus-Tsangpo suture zone. In addition, two younger grains with 57 Ma and 55 Ma ages may indicate a contribution from the Kohistan-Ladakh arc. The detrital zircons in the upper Tertiary sequence show the increased input of younger detrital ages <100 Ma, with more pronounced peaks at ~36-58 Ma, ~72-94 Ma and ~102-166 Ma, indicating the strong resemblance to the Asian sources including the Kohistan-Ladakh arc, Karakoram block and Gangdese batholith. This provenance shift, recorded in the upper portion of Patala Formation and becoming more visible in the upper Tertiary clastic sequence (Kuldana and Murree formations), is related to the collision of the Indian and Asian plates in the northwestern Himalayas. Considering the age of the Patala Formation, we suggest that the Indian and Asian plates collided during 57-55 Ma in the northwestern Himalayas, Pakistan.
WOS关键词HF ISOTOPIC CONSTRAINTS ; U-PB AGE ; TECTONIC IMPLICATIONS ; FORELAND BASIN ; SOUTHERN TIBET ; TETHYS HIMALAYA ; HIGH-PRESSURE ; SUTURE ZONE ; SUBDUCTION ; KOHISTAN
资助项目National Natural Science Foundation of China[41490610] ; Chinese Ministry of Science and Technology[2011CB403101] ; International partnership program of the Chinese Academy of Sciences[131551KYSB20200021]
WOS研究方向Geochemistry & Geophysics ; Mineralogy ; Mining & Mineral Processing
语种英语
WOS记录号WOS:000737058400001
出版者MDPI
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; Chinese Ministry of Science and Technology ; Chinese Ministry of Science and Technology ; International partnership program of the Chinese Academy of Sciences ; International partnership program of the Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Chinese Ministry of Science and Technology ; Chinese Ministry of Science and Technology ; International partnership program of the Chinese Academy of Sciences ; International partnership program of the Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Chinese Ministry of Science and Technology ; Chinese Ministry of Science and Technology ; International partnership program of the Chinese Academy of Sciences ; International partnership program of the Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Chinese Ministry of Science and Technology ; Chinese Ministry of Science and Technology ; International partnership program of the Chinese Academy of Sciences ; International partnership program of the Chinese Academy of Sciences
源URL[http://ir.iggcas.ac.cn/handle/132A11/103966]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Qasim, Muhammad; Tanoli, Javed Iqbal
作者单位1.COMSATS Univ Islamabad, Dept Earth Sci, Abbottabad Campus, Abbottabad 22010, Pakistan
2.Chinese Acad Sci, State Key Lab Lithospher Evolut, Inst Geol & Geophys, Beijing 100029, Peoples R China
3.Univ Azad Jammu & Kashmir, Inst Geol, Muzaffarabad 13100, Pakistan
4.Chinese Acad Sci, Inst Tibetan Plateau Res, Bldg 3,Courtyard 16,Lin Cui Rd, Beijing 100101, Peoples R China
5.COMSATS Univ Islamabad, Dept Earth Sci, Abbottabad Campus,Univ Rd, Abbottabad 22044, Pakistan
6.Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
7.Chinese Acad Sci, Key Lab Continental Collis & Plateau Uplift, Inst Tibetan Plateau Res, Beijing 100101, Peoples R China
8.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
9.Inst Space Technol, Islamabad 44000, Pakistan
推荐引用方式
GB/T 7714		 Awais, Muhammad,Qasim, Muhammad,Tanoli, Javed Iqbal,et al. Detrital Zircon Provenance of the Cenozoic Sequence, Kotli, Northwestern Himalaya, Pakistan; Implications for India-Asia Collision[J]. MINERALS,2021,11(12):15.
APA Awais, Muhammad.,Qasim, Muhammad.,Tanoli, Javed Iqbal.,Ding, Lin.,Sattar, Maryam.,...&Pervaiz, Shahab.(2021).Detrital Zircon Provenance of the Cenozoic Sequence, Kotli, Northwestern Himalaya, Pakistan; Implications for India-Asia Collision.MINERALS,11(12),15.
MLA Awais, Muhammad,et al."Detrital Zircon Provenance of the Cenozoic Sequence, Kotli, Northwestern Himalaya, Pakistan; Implications for India-Asia Collision".MINERALS 11.12(2021):15.

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来源：地质与地球物理研究所

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