On the genetic classification and tectonic implications of the Early Yanshanian granitoids in the Nanling Range, South China

Early Yanshanian (Jurassic) granitoids are widespread in the Nanling Range of South China, and are associated with numerous non-ferrous and rare metal mineral deposits. These granitoids consist mainly of slightly peraluminous biotite monzogranites and K-feldspar granites that are closely associated...

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Main Authors: Li, X., Li, W., Li, Zheng-Xiang
Format: Journal Article
Published: Science in China Press/Zhongguo Kexue Zazhishe 2007
Subjects:
Online Access:http://hdl.handle.net/20.500.11937/45378
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author Li, X.
Li, W.
Li, Zheng-Xiang
author_facet Li, X.
Li, W.
Li, Zheng-Xiang
author_sort Li, X.
building Curtin Institutional Repository
collection Online Access
description Early Yanshanian (Jurassic) granitoids are widespread in the Nanling Range of South China, and are associated with numerous non-ferrous and rare metal mineral deposits. These granitoids consist mainly of slightly peraluminous biotite monzogranites and K-feldspar granites that are closely associated in time and space with subordinate amphibole-bearing granites and muscovite- and garnet-bearing granites. In most previous studies, the biotite-bearing granites were classified as crustal transformation-type (corresponding to the S-type) granites which were interpreted to be derived from the regional Paleoproterozoic meta-sedimentary rocks. In this paper, we re-analyze the geochemical characteristics of a number of representative Early Yanshanian Nanling granitoids. There exists a clear negative correlation between SiO2 and P2O5 for the studied granitoids. The Early Yanshanian Nanling granitoid suites (including amphibole-bearing granodiorites->biotite monzogranites->K-feldspar granites->two-mica (muscovite) granites) are metaluminous to slightly peraluminous I-type or fractionated I-type granites. They were derived predominantly from Proterozoic igneous protoliths. The juvenile crust and/or newly mantle-derived materials might also have been involved in some of these granites. In addition, the I- and fractionated I-type granites are closely associated in time and space with minor amount of A-type felsic and mafic volcanic and intrusive rocks as well as alkaline rocks. All these rocks constitute a typical assemblage of anorogenic, intraplate magmatism, suggesting a dominant lithospheric extensional regime for the Nanling Range and neighboring region during the Early Yansanian period.
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spelling curtin-20.500.11937-453782019-02-19T05:35:17Z On the genetic classification and tectonic implications of the Early Yanshanian granitoids in the Nanling Range, South China Li, X. Li, W. Li, Zheng-Xiang Early Yanshanian genetic classification lithosphere extension Nanling Range South China granite Early Yanshanian (Jurassic) granitoids are widespread in the Nanling Range of South China, and are associated with numerous non-ferrous and rare metal mineral deposits. These granitoids consist mainly of slightly peraluminous biotite monzogranites and K-feldspar granites that are closely associated in time and space with subordinate amphibole-bearing granites and muscovite- and garnet-bearing granites. In most previous studies, the biotite-bearing granites were classified as crustal transformation-type (corresponding to the S-type) granites which were interpreted to be derived from the regional Paleoproterozoic meta-sedimentary rocks. In this paper, we re-analyze the geochemical characteristics of a number of representative Early Yanshanian Nanling granitoids. There exists a clear negative correlation between SiO2 and P2O5 for the studied granitoids. The Early Yanshanian Nanling granitoid suites (including amphibole-bearing granodiorites->biotite monzogranites->K-feldspar granites->two-mica (muscovite) granites) are metaluminous to slightly peraluminous I-type or fractionated I-type granites. They were derived predominantly from Proterozoic igneous protoliths. The juvenile crust and/or newly mantle-derived materials might also have been involved in some of these granites. In addition, the I- and fractionated I-type granites are closely associated in time and space with minor amount of A-type felsic and mafic volcanic and intrusive rocks as well as alkaline rocks. All these rocks constitute a typical assemblage of anorogenic, intraplate magmatism, suggesting a dominant lithospheric extensional regime for the Nanling Range and neighboring region during the Early Yansanian period. 2007 Journal Article http://hdl.handle.net/20.500.11937/45378 10.1007/s11434-007-0259-0 Science in China Press/Zhongguo Kexue Zazhishe fulltext
spellingShingle Early Yanshanian
genetic classification
lithosphere extension
Nanling Range
South China
granite
Li, X.
Li, W.
Li, Zheng-Xiang
On the genetic classification and tectonic implications of the Early Yanshanian granitoids in the Nanling Range, South China
title On the genetic classification and tectonic implications of the Early Yanshanian granitoids in the Nanling Range, South China
title_full On the genetic classification and tectonic implications of the Early Yanshanian granitoids in the Nanling Range, South China
title_fullStr On the genetic classification and tectonic implications of the Early Yanshanian granitoids in the Nanling Range, South China
title_full_unstemmed On the genetic classification and tectonic implications of the Early Yanshanian granitoids in the Nanling Range, South China
title_short On the genetic classification and tectonic implications of the Early Yanshanian granitoids in the Nanling Range, South China
title_sort on the genetic classification and tectonic implications of the early yanshanian granitoids in the nanling range, south china
topic Early Yanshanian
genetic classification
lithosphere extension
Nanling Range
South China
granite
url http://hdl.handle.net/20.500.11937/45378