nkysdb: 共著者関連データベース
GUPTA Alok K. 様の 共著関連データベース
+(A list of literatures under single or joint authorship with "GUPTA Alok K.")
共著回数と共著者名 (a list of the joint author(s))
11: GUPTA Alok K.
6: ARIMA Makoto
1: DWIVEDI Mrigank Mauli, HARIYA Yu, HAUKKA M.T., KAR Ruchira, LEMAITRE R.W., ONUMA Kosuke, PATI Jayanta K., SINGH Puniti, 八木 健三, 有馬 真
発行年とタイトル (Title and year of the issue(s))
1976: Experimental Investigations on Some Synthetic Leucite Rocks under Water Vapor Pressures
1978: Experimental Study on the Forsterite Grossularite Incompatibility
1978: 擬白榴石の成因に関する一考察 とくにソ連Tezhsarsk産擬白榴石を中心に
On the Genesis of Pseudoleucite with Reference to the Psudoleucite from Tezhsarsk, USSR
1983: Geochemical Studies on the Carbonated Apatite Glimmerites from Damodar Valley, India
1998: 水の存在下，1, 10 および20 kbar, 750℃における金雲母 マンガン金雲母系の安定関係
Experimental studies on the system phlogopite manganese phlogopite at 1, 10 and 20 kbar and 750 degrees C in presence of excess water under NNO buffer conditions
2000: Experimental study of the system diopside albite nepheline at P(H2O)=P(Total)=2 and 10 kbar and at P(Total)=28 kbar
2000: Phase equilibrium constraints on the petrogenesis of nephelinites with reference to the system diopside nepheline under variable P T conditions in the presence or absence of water
2003: Experimental Study of the System Forsterite Akermanite Leucite at P(H2O)=P(Total)=23 kbar and Variable Temperatures and its Significance in the Genesis of Potassium Rich Mafic and Ultramafic Rocks (V05/04A/A01 009)
2004: Experimental Study of the System Forsterite Diopside Leucite under 1 and 23 kb [(P(H2O) = P(Total)] at Variable Temperatures and Its Significance (99 22)(poster sesseion)
2007: An experimental study of the joins leucite akermanite albite and leucite akermanite albite50anorthite50 at atmospheric pressure and 1 GPa (H2O saturated conditions): Its significance in the leucite sodic plagioclase and melilite plagioclase incompatibilities
2007: Experimental study of the joins forsterite diopside leucite and forsterite leucite akermanite up to 2.3 GPa [P(H2O)=P(Total)] and variable temperatures: Its petrological significance
