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
Though Li isotope fractionation during mantle melting and differentiation of basaltic melts have been proved insignificant, Li isotopic systems during crustal processes remain unclear. To study this, we report combined petrological, Nd-Sr and Li isotopic data for the late Paleozoic coexisting I- and...
Main Authors: | , , , |
---|---|
Format: | Article |
Language: | English |
Published: |
Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust
2017-09-01
|
Series: | Геодинамика и тектонофизика |
Online Access: | https://www.gt-crust.ru/jour/article/view/394 |
_version_ | 1797855770058948608 |
---|---|
author | Bin Chen Keke Sun Chao Huang Hai-ou Gu |
author_facet | Bin Chen Keke Sun Chao Huang Hai-ou Gu |
author_sort | Bin Chen |
collection | DOAJ |
description | Though Li isotope fractionation during mantle melting and differentiation of basaltic melts have been proved insignificant, Li isotopic systems during crustal processes remain unclear. To study this, we report combined petrological, Nd-Sr and Li isotopic data for the late Paleozoic coexisting I- and A-type granites in the East Junggar orogen of the Central Asian Orogenic Belt. The granites were formed responding to underplating of mafic magmas in the lower crust in a postcollisional, extensional regime, and intruded into the Paleozoic foldbelts that formed due to extensive oceanic subduction-accretion processes. |
first_indexed | 2024-04-09T20:29:17Z |
format | Article |
id | doaj.art-bafead5e5d204ee786123f2a727fd1f8 |
institution | Directory Open Access Journal |
issn | 2078-502X |
language | English |
last_indexed | 2024-04-09T20:29:17Z |
publishDate | 2017-09-01 |
publisher | Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust |
record_format | Article |
series | Геодинамика и тектонофизика |
spelling | doaj.art-bafead5e5d204ee786123f2a727fd1f82023-03-30T20:08:02ZengRussian Academy of Sciences, Siberian Branch, Institute of the Earth's crustГеодинамика и тектонофизика2078-502X2017-09-018342943010.5800/GT-2017-8-3-0253253LITHIUM 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 ANATEXISBin Chen0Keke Sun1Chao Huang2Hai-ou Gu3Hefei University of TechnologyPeking UniversityHefei University of TechnologyHefei University of Technology University of Science and TechnologyThough Li isotope fractionation during mantle melting and differentiation of basaltic melts have been proved insignificant, Li isotopic systems during crustal processes remain unclear. To study this, we report combined petrological, Nd-Sr and Li isotopic data for the late Paleozoic coexisting I- and A-type granites in the East Junggar orogen of the Central Asian Orogenic Belt. The granites were formed responding to underplating of mafic magmas in the lower crust in a postcollisional, extensional regime, and intruded into the Paleozoic foldbelts that formed due to extensive oceanic subduction-accretion processes.https://www.gt-crust.ru/jour/article/view/394 |
spellingShingle | Bin Chen Keke Sun Chao Huang Hai-ou Gu 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 |
title | 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 |
title_full | 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 |
title_fullStr | 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 |
title_full_unstemmed | 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 |
title_short | 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 |
title_sort | 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 |
url | https://www.gt-crust.ru/jour/article/view/394 |
work_keys_str_mv | AT binchen lithiumisotopicconstraintsontheoriginofiandatypegranitesfromeastjunggarnwchinaofthecentralasianorogenicbeltimplicationsforliisotopicfractionationduringcrustalanatexis AT kekesun lithiumisotopicconstraintsontheoriginofiandatypegranitesfromeastjunggarnwchinaofthecentralasianorogenicbeltimplicationsforliisotopicfractionationduringcrustalanatexis AT chaohuang lithiumisotopicconstraintsontheoriginofiandatypegranitesfromeastjunggarnwchinaofthecentralasianorogenicbeltimplicationsforliisotopicfractionationduringcrustalanatexis AT haiougu lithiumisotopicconstraintsontheoriginofiandatypegranitesfromeastjunggarnwchinaofthecentralasianorogenicbeltimplicationsforliisotopicfractionationduringcrustalanatexis |