TY - JOUR
T1 - Anatexis and cooling history of granitic gneiss in the Xitieshan Terrane, North Qaidam: Evidence from 40Ar/39Ar geochronological study of leucosome
AU - Hu, R.
AU - Qiu, H.N.
AU - Wijbrans, J.R.
AU - Brouwer, F.M.
AU - He, L.
AU - Wang, M.
PY - 2016
Y1 - 2016
N2 - Felsic leucosome veins are widely distributed in biotite granitic gneiss in the Xitieshan terrane, North Qaidam, western China. The leucosome veins are derived from anatectic magmatites and consist mainly of plagioclase, K-feldspar, quartz and amphibole with minor biotite. Thermobarometric study indicates that the leucosome records granulite-facies metamorphic conditions of P=(6.5-9.6)×10
AB - Felsic leucosome veins are widely distributed in biotite granitic gneiss in the Xitieshan terrane, North Qaidam, western China. The leucosome veins are derived from anatectic magmatites and consist mainly of plagioclase, K-feldspar, quartz and amphibole with minor biotite. Thermobarometric study indicates that the leucosome records granulite-facies metamorphic conditions of P=(6.5-9.6)×10
UR - https://www.scopus.com/pages/publications/84964407300
UR - https://www.scopus.com/inward/citedby.url?scp=84964407300&partnerID=8YFLogxK
U2 - 10.16539/j.ddgzyckx.2016.01.011
DO - 10.16539/j.ddgzyckx.2016.01.011
M3 - Article
SN - 1006-513X
SP - 125
EP - 135
JO - Geotectonica et Metallogenia
JF - Geotectonica et Metallogenia
IS - 40
M1 - 1
ER -