supported by the National Natural Science Foundation of China(Nos.41906048 and 91858215).
We applied double-difference tomography to relocate seismic events and determine the lithospheric velocity structure beneath the New Britain Island arc and the South Bismarck Sea Basin,based on the local P wave arriva...
supported by the National Key Basic Research Program of China (No. 2013CB429700);the National Natural Science Foundation of China (Nos. 4132 5021, 41306053, 40476044);the Strategic Priority Research Program of the Chinese Academy of Sciences (No XDA11030302);the Special Fund for the Taishan Scholar Program of Shandong Province (No. ts201511061);the AoShan Talents Program Supported by Qingdao Nationa Laboratory for Marine Science and Technology (No. 2015 ASTP-0S17);the Innovative Talent Promotion Program (No. 2012RA2191);the Science and Technology Devel opment Program of Shandong Province (No. 2013GRC 31502);the Scientific and Technological Innovation Project Financially Supported by Qingdao National Labora tory for Marine Science and Technology (No. 2015ASKJ 03);the National High Level Talent Special Support Program;the CAS/SAFEA International Partnership Program for Creative Research Teams;the Qingdao Collaborative Innovation Center of Marine Science and Technology
There has been much recent interest in the origin of intermediate lava and several hypotheses are: 1) direct melting of the mantle under water-saturated conditions, 2) partial melting of altered crust, 3) fractional c...
supported by the National Key Basic Research Program of China (Grant No. 2013CB429700);National Natural Science Foundation of China (Grant Nos. 40976027, 40830849 and 40906029);Shandong Province Natural Science Foundation for Distinguished Young Scholars (Grant No. JQ200913)
This paper reports silicon and oxygen isotopes of 20 kinds of igneous rocks and their major elements from the eastern Manus Basin. Combining silicon and oxygen isotopic data from other studies, we suppose that both δ...