LITHIUM ISOTOPIC CONSTRAINTS ON THE ORIGIN OF I- AND A-TYPE GRANITES FROM EAST JUNGGAR (NW CHINA) OF THE CENTRAL ASIAN OROGENIC BELT: IMPLICATIONS FOR LI ISOTOPIC FRACTIONATION DURING CRUSTAL ANATEXIS
https://doi.org/10.5800/GT-2017-8-3-0253
Аннотация
Об авторах
Bin ChenКитай
School of Resources and Environmental Engineering,
Hefei 230009
Keke Sun
Китай
School of Earth and Space Sciences,
Beijing 100871
Chao Huang
Китай
School of Resources and Environmental Engineering,
Hefei 230009
Hai-ou Gu
Китай
School of Resources and Environmental Engineering, Hefei 230009;
School of Earth and Space Sciences, Hefei 230026
Рецензия
Для цитирования:
Chen B., Sun K., Huang Ch., Gu H. LITHIUM ISOTOPIC CONSTRAINTS ON THE ORIGIN OF I- AND A-TYPE GRANITES FROM EAST JUNGGAR (NW CHINA) OF THE CENTRAL ASIAN OROGENIC BELT: IMPLICATIONS FOR LI ISOTOPIC FRACTIONATION DURING CRUSTAL ANATEXIS. Геодинамика и тектонофизика. 2017;8(3):429-430. https://doi.org/10.5800/GT-2017-8-3-0253
For citation:
Chen B., Sun K., Huang Ch., Gu H. LITHIUM ISOTOPIC CONSTRAINTS ON THE ORIGIN OF I- AND A-TYPE GRANITES FROM EAST JUNGGAR (NW CHINA) OF THE CENTRAL ASIAN OROGENIC BELT: IMPLICATIONS FOR LI ISOTOPIC FRACTIONATION DURING CRUSTAL ANATEXIS. Geodynamics & Tectonophysics. 2017;8(3):429-430. https://doi.org/10.5800/GT-2017-8-3-0253