首页|Principle of Hydrogen Isotope Geochemistry Paleo-altimeter and its Potential in Reconstructing Paleo-elevation of the Southeastern Tibetan Plateau

Principle of Hydrogen Isotope Geochemistry Paleo-altimeter and its Potential in Reconstructing Paleo-elevation of the Southeastern Tibetan Plateau

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The reconstruction of paleo-elevation serves a dual purpose to enhance our comprehension of geodynamic processes affecting terrestrial landforms and to contribute significantly to the interpretation of atmospheric circulation and biodiversity.The oxygen(δ18Ow)and deuterium(δDw)isotopes in atmospheric precipitation are systematically depleted with the increase of altitude,which are typical and widely applicated paleo-altimeters.The utilization of hydrogen isotope of hydrous silicate minerals within the shear zone system,volcanic glass,and plant leaf wax alkanes offers valuable insights for addressing evaporation and diagenesis.In this paper,we review the principle,application conditions,and influencing factors of the hydrogen isotope paleo-altimeter.In addition,we discuss the feasibility of utilizing this technique for quantitatively estimating the paleo-elevation of the southeastern Tibetan Plateau,where multiple shear zones extend over hundred kilometers parallel to the topographic gradient.

paleo-elevationhydrogen isotopehydrous silicate mineralsvolcanic glassTibetan Plateau

CUI Fengzhen、LIU-ZENG Jing、LI Yunshuai、XU Qiang、TANG Maoyun、WANG Heng、SUN Zhaotong

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School of Earth System Science,Tianjin University,Tianjin 300072,China

State Key Laboratory of Earthquake Dynamics,Institute of Geology,China Earthquake Administration,Beijing 100029,China

School of Earth Science and Technology,Southwest Petroleum University,Chengdu 610500,China

Chongqing Earthquake Agency,Chongqing 401147,China

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National Key Research and Development program of ChinaNational Natural Science Foundation of ChinaNational Natural Science Foundation of ChinaState Key Laboratory of Earthquake Dynamics,Institute of Geology,China Earthquake Administration

2021YFC30006044203030542272257LED2022B04

2024

地质学报(英文版)
中国地质学会

地质学报(英文版)

CSTPCD
影响因子:1.414
ISSN:1000-9515
年,卷(期):2024.98(4)