supported by a RFBR-TUBITAK grant(Project No.09-05-91220-ST-a;co-leaders E.Sharkov and M.Keskin);Scientific Project of IGM SB RAS;Ministry of Education and Science(Russia)Project No 14.B25.31.0032;JSPS Grant-in-Aid No.14526
The Caucasian-Arabian belt is part of the huge late Cenozoic Alpine-Himalayan orogenic belt formed by collision of continental plates. The belt consists of two domains: the Caucasian-Arabian Syntaxis (CAS) in the s...
financial support from Department of Science and Technology, New Delhi in the form of research grant (ESS/16/295/2006) to KRH and NVCR is acknowledged
Two petrologically distinct alkali feldspar syenite bodies (AFS-1 and AFS-2) from Chhotaudepur area, Deccan Large Igneous Province are reported in the present work. AFS-1 is characterized by hypidio-morphic texture ...
the People’s Republic of China(Grant Nos.2002CB412601,G1999043202);the Knowledge Innovation Program of Chinese Academy of Sciences(Grant Nos.KZCX2-102,KZCX2-SW-117 , KZCX3-SW-122);the National Climbing Program of China(Grant No.95-Y-25); theNational Natural Science Foundation of China(Grant Nos.40273019,40172028).
Petrology, element and isotopic geochemistry of the Mesozoic intrusive rocks in the Tongling area were systematically investigated in this study. The intrusive rocks can be divided into two groups, one contains shosho...
the "973" Project (Grant No. G1998040800) and the National Natural Science Foundation of China (Grant No. 49732070).
Two periods of magma activities, i.e. 106-112 Ma shoshonitic eruption and 82 Ma trachytic intrusion, are recognized at the intersection of the Altyn Tagh fault and the northern marginal fault of the Qilian terrane, no...
It is known that large amounts of Cenozoic high potassium volcanic rocks occur on the Tibetan plateau. The question is where do those high potassium magmas come from? Since the plateau is being compressed by subductio...