financial support as JRF&SRF(Fellowship letter No.23/12/2012(ii)EU-V)
High resolution shallow seismic data was acquired from inner continental shelf of Goa,west coast of India to map underlying stratigraphic and buried geomorphic features of shelf strata.Seismic data revealed characteri...
financially supported by the National Science and Technology Major Project(Grant No.2011ZX05008-001);the National Natural Science Foundation of China(Grant No.40739906);the Chinese State 973 Project(Grant No.2011CB201100)
The Hala'alat Mountains are located at the transition between the West Junggar and the Junggar Basin. In this area, rocks are Carboniferous, with younger strata above them that have been identified through well data ...
fnancially supported by the National Key Project of Science and Technology for Development of Large-size Oil&Gas Fields and Coal-bed Gas(Grant No.2008ZX05003-002);by the State Key Laboratory of Petroleum Resources and Prospecting(No.prp2009-02);The study is a contribution to IGCP#592 Project
The unconformity surface at the bottom of the Paleogene is one of the most important migration pathways in the Sikeshu Sag of the Junggar Basin,which consists of three layers:upper coarse clastic rock,lower weatherin...
the supports in part of KAKENH1(Grant Nos. 23540560 and 24840020)
The Earth was born from a giant impact at 4.56 Ga. It is generally thought that the Earth subsequently cooled, and hence shrunk, over geologic time. However, if the Earth's convection was double-layered, there must h...