Heat Aggregation Mechanisms of Hot Dry Rocks Resources in the Gonghe Basin, Northeastern Tibetan Plateau-Reference-Cited by-同舟云学术

Heat Aggregation Mechanisms of Hot Dry Rocks Resources in the Gonghe Basin, Northeastern Tibetan Plateau

Published:2021-12 Issue:6 Volume:95 Page:1793-1804
ISSN:1000-9515
Container-title:Acta Geologica Sinica - English Edition
language:en
Short-container-title:Acta Geologica Sinica (Eng)

Author:

LIN Wenjing¹²,WANG Guiling¹²,ZHANG Shengsheng³,ZHAO Zhen⁴,XING Linxiao¹²,GAN Haonan¹²,TAN Xianfeng⁵

Affiliation:

1. Institute of Hydrogeology and Environmental Geology Chinese Academy of Geological Sciences Shijiazhuang 050061 China

2. Technical Innovation Center for Geothermal and HDR Exploration and Development Ministry of Natural Resources Shijiazhuang 050061 China

3. Institute of the Hydrogeology and Engineering Geology of Qinghai Xining 810008 China

4. Qinghai Bureau of Environmental Geology Exploration Xining 810007 China

5. Shandong Provincical Lunan Geo‐engineering Exploration Institute (The Second Geological Brigade of Shandong Geological Exploration Bureau), Jining Shandong 272100 China

Funder

National Key Research and Development Program of China

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/1755-6724.14873

Reference48 articles.

1. Bullard E.C. 1939.Heat Flow in South Africa. Proceedings of the Royal Society of London A 474–502.

2. Global map of solid Earth surface heat flow

3. High heat flow in southern Tibet

4. Partially melted, mica-bearing crust in Central Tibet

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