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Date:December 3rd, 2019
Location:3rd floor conference room, Building 3 (the State Key Laboratory of Ore Deposit Geochemistry), IGCAS |
Paul Robinson
What can ophiolite-hosted diamonds tell us about the origin of podiform chromitites? |
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ZHOU Meifu
Genesis of the Jinchuan Cu-Ni deposit |
Sasha Aleksandr Stepanov
Origin of rare metal granites/pegmatites: role of fractional crystallisation of mica and monazite |
Dan Harlov
IOA deposits of the Middle to Lower Yangtze River Metallogenic Belt |
Punya Charusiri
Distributions of igneous rocks and their associated mineralization in the Sukhothai Fold Belt, Thailand |
LI Yang
A Metal Rhythm under Absolute and Relative Timeframes |
CAO Mingjian
Magmatic and hydrothermal formation processes at Black Mountain porphyry Cu-Au deposit, Philippines: Insights from mineral chemistry and implications for mineralization |
ZHANG Rongqing
Granite-related tin deposits in the Youjiang Basin, South China |
DING Xin
Iron isotopic characteristics of magmatic Ni-Cu sulfide deposit: an example from Lengshuiqing, SW China |
LIWeiqiang
Understanding mineralization using metal stable isotopes: new developments |
SONG Xieyan
Chromite geochemistry implication on magma generatin associated with magmatic sulfide mineralizstion |
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DU Wei
Exolution of pyrope-grossular garnet at high pressure and high temperature |
