the Scientific Project of Ministry of Land and Resource of China;the National Natural Science Foundation of China;the Doctoral Station Foundation of Ministry of Education of China
The pressure gradient of the lithosphere is a key to explaining various geological processes, and varies also in time and space similar to the geothermal gradient. In this paper a correlation formula of geothermal gra...
The boundary between lithosphere and asthenosphere essentially represents a thermal boundary (the solidus). Temperature variation across this boundary can lead to the change of lithosphere thickness. In the case of el...
Based on data from petrochemistry, trace element geochemistry and isotopic compositions of Mesozoic-Cenozoic volcanic rocks in three basins in the Bohai region, some conclusions can be drawn. In the region. there are ...
The Tibetan lithosphere plays an important role in global geodynamics, Geophysical evidence from gravity, geoidal, seismic, geothermal, and magnetotelluric (MT) observations provides important insights on the structur...
Mesozoic and Cenozoic basalitc rnagmatism within the basins around Bohai area displays temporal variations in petrochemistry,trace element and isotope geochmistry. Two stages of evolution are recognized. The preextens...