Shengbiao Hu

Chinese Academy of Sciences

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Yuntao Tian

Sun Yat-sen University

Guangzheng Jiang

Chengdu University of Technology

Yibo Wang

Czech Academy of Sciences, Institute of Physics

Lijuan He

Chinese Academy of Sciences

Yizuo Shi

Research Institute of Petroleum Exploration and Development

Zhuting Wang

Anhui University of Science and Technology

Barry P. Kohn

University of Melbourne

Xiaoyin Tang

China Geological Survey

Andrew Gleadow

University of Melbourne

Shuchun Yang

Guangdong-Hongkong-Macau Joint Laboratory of Collaborative Innovation for Environmental Quality

Cooperative Institutions

Chinese Academy of Sciences

University of Chinese Academy of Sciences

Institute of Geology and Geophysics

China Geological Survey

Sun Yat-sen University

China University of Petroleum, Beijing

State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation

Sinopec (China)

Research Institute of Petroleum Exploration and Development

Chengdu University of Technology

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Thermo-rheological structure of the northern margin of the South China Sea: Structural and geodynamic implications

Tectonophysics (2020)

Jie Hu Yuntao Tian Zulie Long Di Hu Yu‐Ping Huang

Peridotite

Passive margin

Continental Margin

10.1016/j.tecto.2020.228338

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Citations (8)

Thermal history and tectonic subsidence of the Bohai Basin, northern China: a Cenozoic rifted and local pull-apart basin

Physics of The Earth and Planetary Interiors (2001)

Shengbiao Hu Paul B. O’Sullivan Asaf Raza Barry P. Kohn

Thermal subsidence

Fission track dating

Tectonic subsidence

Pull apart basin

Tectonic uplift

10.1016/s0031-9201(01)00257-6

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Citations (260)

Heat flow study at the Chinese Continental Scientific Drilling site: Borehole temperature, thermal conductivity, and radiogenic heat production

Journal of Geophysical Research Atmospheres (2008)

Lijuan He Shengbiao Hu Shaopeng Huang Wencai Yang Jing Wang

The Chinese Continental Scientific Drilling (CCSD) Project offers a unique opportunity for studying the thermal regime of the Dabie‐Sulu ultrahigh‐pressure metamorphic belt. In this paper, we report measurements of borehole temperature, thermal conductivity, and radiogenic heat production from the 5158 m deep main hole (CCSD MH). We have obtained six continuous temperature profiles from this borehole so far. The temperature logs show a transient mean thermal gradient that has increased from 24.38 to 25.28 K km −1 over a period of about 1.5 years. We measured thermal conductivities and radiogenic heat productions on more than 400 core samples from CCSD MH. The measured thermal conductivities range between 1.71 and 3.60 W m −1 K −1 , and the radiogenic heat productions vary from 0.01 μ W m −3 to over 5.0 μ W m −3 , with a mean value of 1.23 ± 0.82 μ W m −3 for the upper 5‐km layer of the crust. The heat productions in CCSD MH appear to be more rock‐type than depth‐dependent and, over the depth range of CCSD MH, do not fit the popular model of heat production decreasing exponentially with increasing depth. The measured heat flow decreases with depth from ∼75 mW m −2 near the surface to ∼66 mW m −2 at a depth of 4600 m. High heat flow anomalies occur at ∼1000 and ∼2300 m, and low anomalies occur at 3300–4000 m. A preliminary two‐dimensional numerical model suggests that both radiogenic heat production and thermal refraction due to structural heterogeneity are at least partially responsible for the vertical variation of heat flow in CCSD MH.

Radiogenic nuclide

Scientific drilling

Heat flow

10.1029/2007jb004958

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Citations (76)

Data tables and supporting information for the paper entitled “Ground surface temperature history since 20 kyr BP in Northeast Asia: Reconstructions from the borehole geotherms of the International Continental Scientific Drilling Project (ICDP) SK-2e”

Figshare (2023)

Guangzheng Jiang Yuntao Tian Qingtian Lv Mike Sandiford Yizuo Shi

Scientific drilling

10.6084/m9.figshare.22273054.v1

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Citations (0)

Effect of different exploitation schemes on production performance from the carbonate reservoir: A case study in Xiong'an new area

Journal of Cleaner Production (2021)

Zhuting Wang Chao Zhang Guangzheng Jiang Yibao Wang Shengbiao Hu

10.1016/j.jclepro.2021.128050

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Citations (12)

Geothermal constraints on Emeishan mantle plume magmatism: paleotemperature reconstruction of the Sichuan Basin, SW China

International Journal of Earth Sciences (2016)

Chuanqing Zhu Shengbiao Hu Nansheng Qiu Qiang Jiang Song Rao

Large igneous province

Mantle plume

10.1007/s00531-016-1404-2

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Citations (45)

Provenance evolution of the Fushan Sag (Hainan Island, Southern China): constraints from U-Pb geochronology on detrital zircons

Marine and Petroleum Geology (2024)

Qiqi Song Jie Hu Lei Dong Zhiwu Li Rong Tang

Geochronology

10.1016/j.marpetgeo.2024.107037

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The eastern Tibetan Plateau geothermal belt, western China: Geology, geophysics, genesis, and hydrothermal system

Tectonophysics (2017)

Xian-Chun Tang Jian Zhang Zhonghe Pang Shengbiao Hu Jiao Tian

Fumarole

10.1016/j.tecto.2017.08.035

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Citations (73)

Recent studies on hydrothermal systems in China: a review

Geothermal Energy (2014)

Yanlong Kong Zhonghe Pang Haibing Shao Shengbiao Hu Olaf Kolditz

This paper reviews the state-of-the-art in hydrothermal systems in China with emphasis on current studies of potential and reservoir engineering. Three hydrothermal systems, namely, Yangbajing, Xianyang, and Xiongxian, are used as case studies to represent high temperature granite reservoirs, medium-to-low temperature sandstone reservoirs, and medium-to-low temperature carbonate reservoirs, respectively. There is a huge potential of hydrothermal resources in China that have not been fully studied for possible exploitation. The study reveals that the potential of developing hydrothermal resources is preferable to exploitation of hot-dry-rock (HDR) systems in the near future. In order to enhance the utilization efficiency and prolong the economic lifetime of a geothermal field, reinjection needs to be increased, including treated wastewater as an option. In this regard, deep karstic aquifers containing hot water are the most ideal targets for development due to their favorable characteristics including high single-well yield, low salinity, easy reinjection, and fewer environmental impacts when exploited. The next challenge lies in the geothermal reservoir management for sustainable production. Numerical models describing the full complexity of coupled physicochemical thermodynamic processes such as the open source OpenGeoSys modeling platform are powerful tools for production planning as well as for assessing the possible environmental impacts. Comprehensive reservoir simulation should be employed to provide an optimal fluid production scheme and to maximize the sustainability in the development of a hydrothermal field.

10.1186/s40517-014-0019-8

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Citations (67)

Provenance of the Paleogene sediments in the Pearl River Mouth Basin, northern South China Sea: Insights from zircon U-Pb and fission track double dating

Journal of Asian Earth Sciences (2020)

Xiaoyin Tang Shuchun Yang Shengbiao Hu

Paleogene

Fission track dating

River mouth

10.1016/j.jseaes.2020.104494

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Citations (12)