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DOI | 10.1002/tect.20086 |
Evidence for constriction and Pliocene acceleration of east-west extension in the North Lunggar rift region of west central Tibet | |
Sundell, Kurt E.; Taylor, Michael H.; Styron, Richard H.; Stockli, Daniel F.; Kapp, Paul; Hager, Christian; Liu, Deliang; Ding, Lin | |
通讯作者 | Sundell, KE (通讯作者) |
发表日期 | 2013 |
ISSN | 0278-7407 |
EISSN | 1944-9194 |
起始页码 | 1454 |
结束页码 | 1479 |
卷号 | 32期号:5 |
英文摘要 | The active north trending North Lunggar rift in west central southern Tibet exposes an extensional metamorphic core complex bounded by an east dipping low-angle normal fault. Apatite and zircon (U-Th)/He thermochronology and thermal modeling of the North Lunggar rift document a minimum timing for rift inception at >10Ma and rapid footwall exhumation between 5 and 2Ma. Miocene footwall cooling and exhumation rates were initially slow to moderate at <50 degrees CMa(-1) and <1mma(-1), followed by increased Pliocene rates as high as >400 degrees CMa(-1) and 4-10mma(-1). Footwall isotherms were significantly compressed during rapid exhumation resulting in an elevated transient geothermal gradient between 50 and 90 degrees Ckm(-1). The minimum magnitude of horizontal extension for the North Lunggar rift is 8.1-12.8km; maximum is 15-20km, less in the south at similar to 10km. Mean Pliocene extension rate is 1.2-2.4mma(-1) in the similar to 120 degrees direction. Results for the North Lunggar rift are similar in magnitude, rate, and orientation of slip to the kinematically linked Lamu Co dextral strike-slip fault to the north. This suggests a state of constrictional strain during Pliocene time along this stretch of the Bangong-Nujiang suture from which the Lamu Co fault emanates. The onset of extension in this region may be explained by crustal thickening and gravitational orogenic collapse, followed by accelerated rifting resulting from localized crustal stretching and increased magmatic activity, potentially driven by the position and northward extent of underthrusting Indian lithosphere. |
关键词 | LOW-TEMPERATURE THERMOCHRONOMETRYMETAMORPHIC CORE COMPLEXESAPATITE (U-TH)/HE THERMOCHRONOMETRYINDIA-ASIA COLLISIONNUJIANG SUTURE ZONESOUTHERN TIBETTECTONIC EVOLUTIONLOWER CRUSTQUATERNARY EXTENSIONDIFFUSION KINETICS |
英文关键词 | Tibet; North Lunggar; rift acceleration; low-angle normal faulting; (U-Th); He thermochronology; transient geothermal gradient |
语种 | 英语 |
WOS研究方向 | Geochemistry & Geophysics |
WOS类目 | Geochemistry & Geophysics |
WOS记录号 | WOS:000327305800023 |
来源期刊 | TECTONICS
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来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/258213 |
推荐引用方式 GB/T 7714 | Sundell, Kurt E.,Taylor, Michael H.,Styron, Richard H.,et al. Evidence for constriction and Pliocene acceleration of east-west extension in the North Lunggar rift region of west central Tibet[J]. 中国科学院青藏高原研究所,2013,32(5). |
APA | Sundell, Kurt E..,Taylor, Michael H..,Styron, Richard H..,Stockli, Daniel F..,Kapp, Paul.,...&Ding, Lin.(2013).Evidence for constriction and Pliocene acceleration of east-west extension in the North Lunggar rift region of west central Tibet.TECTONICS,32(5). |
MLA | Sundell, Kurt E.,et al."Evidence for constriction and Pliocene acceleration of east-west extension in the North Lunggar rift region of west central Tibet".TECTONICS 32.5(2013). |
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