terrestrial heat flow
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Author(s):  
Suze Nei Pereira Guimarães ◽  
Elias Martins Guerra Prado ◽  
Fábio Pinto Vieira ◽  
Christian Michel Lacasse ◽  
Nina da Silva Rocha ◽  
...  

Geothermics ◽  
2021 ◽  
Vol 96 ◽  
pp. 102210
Author(s):  
Zhuting Wang ◽  
Song Rao ◽  
Hongping Xiao ◽  
Yibo Wang ◽  
Guangzheng Jiang ◽  
...  

Author(s):  
Jorge Luiz dos Santos Gomes ◽  
Valiya Mannathal Hamza ◽  
Alan Jessop ◽  
Massimo Verdoya

Editorial


Geothermics ◽  
2021 ◽  
Vol 90 ◽  
pp. 101993
Author(s):  
Massimo Verdoya ◽  
Paolo Chiozzi ◽  
Gianluca Gola

Geothermics ◽  
2020 ◽  
Vol 86 ◽  
pp. 101799 ◽  
Author(s):  
Jiong Zhang ◽  
Shaopeng Huang ◽  
Yinhui Zuo ◽  
Yongshui Zhou ◽  
Zhi Liu ◽  
...  

2020 ◽  
Vol 32 (6) ◽  
pp. 1328-1346
Author(s):  
Yinhui Zuo ◽  
Shu Jiang ◽  
Shihu Wu ◽  
Wei Xu ◽  
Jiong Zhang ◽  
...  

Geothermics ◽  
2020 ◽  
Vol 83 ◽  
pp. 101709
Author(s):  
Yuchen Liu ◽  
Nansheng Qiu ◽  
Huili Li ◽  
Anlai Ma ◽  
Jian Chang ◽  
...  

Energies ◽  
2019 ◽  
Vol 12 (24) ◽  
pp. 4608
Author(s):  
Yue Cui ◽  
Chuanqing Zhu ◽  
Nansheng Qiu ◽  
Boning Tang ◽  
Sasa Guo

Herein, integrated heat production analysis in the Xiong’an area was conducted by measuring uranium, thorium, and potassium in different rock types to clarify crust heat flow contribution, simulate the conductive terrestrial heat flow, and illustrate heat source mechanisms of Xiong’an area geothermal resources. The study area was divided into three lithosphere structure types from west to east, and heat production corresponded to layer thickness and heat production with the central area having thicker crust and lower heat production than the eastern and western areas. Crustal heat production, mantle heat flow, and crust–mantle heat flow ratio reveal a ‘cold crust-hot mantle’ in the Xiong’an area.


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