supported by the National Natural Science Foundation of China(No.42072050);the Science Fund for Distinguished Young Scholars of Hubei Province(No.2020CFA104)。
Water in the deep Earth’s interior has important and profound impacts on the geodynamical properties at high-temperature(T)and high-pressure(P)conditions.A series of dense hydrous Mg-silicate(DHMS)phases are generate...
supported by the National Natural Science Foundation of China (Grants Nos. 41902242);the Geological Survey Projects Foundation of the Institute of Hydrogeology and Environmental Geology (Grants Nos. DD20190303, DD20221773)。
The geothermal resources in Fujian Province are mainly hydrothermal resources of medium-low temperature.To better understand the whole process and conditions of heat control in the middle and deep crust,this study foc...
Artificial Neural Networks(ANNs)are used in numerous engineering and scientific disciplines as an automated approach to resolve a number of problems.However,to build an artificial neural network that is prudent enough...
The Fourier equation explains the dynamics of heat transfer. But bringing this phenomenon closer to the notion of fibration seems difficult to achieve. This study then aims to find the solution of the one-dimensional ...
supported by the National Natural Science Foundation of China (Nos.41530319,41374079,41374060);the State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences (No.MSFGPMR201309)
Knowledge of heat flow and associated variations of temperature with depth is crucial for understanding how the Earth functions. Here, we demonstrate possible heat shielding effects that result from the occurrence of ...
supported by the Fundamental Research Funds for the Central Universities (Grant Nos. 2652013021 and2010ZD15)
The lithosphere temperature beneath the Tibetan plateau was estimated by local isostasy equilib- rium constrained geothermal calculation. Maps of the lateral temperature variation at depths of 40 km, 70 km, and Moho a...
supported by the 973 Research Project(Grant no. 2008CB425704) from the Ministry of Science and Technology,PRC;the National Natural Science Foundation of China(Grant nos 40572128,40376013,40104003);the Fundamental Research Funds for the Central Universities(Grant nos 2010ZD15 and 2010ZY23)
The temperature distributions of the lithosphere underneath the mainland of China were estimated by applying local isostatic equilibrium-constrained geothermal calculations. Maps of the lateral temperature variation a...
supported by the Knowledge Inno-vation Project of the Chinese Academy of Sciences (No. KZCX2-YW-Q08-3-6);the National Natural Science Founda-tion of China (Nos. 90714001, 40773015);the CAS/SAFEA International Partnership Program for Creative Research Teams (No. KZCX2-YW-Q04-06)
Application of reliable thermobarometer on garnet-bearing mantle xenoliths and granulite xenoliths entrained by Cenozoic basalts in eastern China reveals two main types of geotherm. The first type, as exampled by Hann...
supported by grants from the National Natural Science Foundation of China(No.40104003);China Post-doctoral Science Foundation;the Chinese Academy of Sciences K.C.Wong Post-doctoral Research Award
On the basis of a one-by-one latitude-longitude grid three-dimensional seismic velocity model, the crustal P-wave velocity structure in eastern China (105-125°E and 18-41°N) is obtained, and a set of geotherms for e...