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...

Full description

Bibliographic Details
Main Authors: Bin Chen, Keke Sun, Chao Huang, Hai-ou Gu
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