Journal:Journal of Earth Science
Place of Publication:China
Abstract:Geochronological and geochemical analyses were performed on K-feldspar granites and monzonitic granites from the Xilinhot area, Inner Mongolia, China. Zircon U/Pb ages indicate that the two types granites were emplaced during the Lower Carboniferous. The K-feldspar granites (332 Ma) have the typical A-type granite characteristics of a post-collision setting. The monzonitic granites have an emplacement age of 323 Ma. Zircon εHf values of the former range from +12.8 to +14.2, with an average TDM2 of 453 Ma.
Co-author:Zhao Xiaocheng; Zhou Wenxiao; Fu Dong; Huang Bo; Li Ziqian; Ge Mengchun,
First Author:Zhao Xiaocheng
Indexed by:Journal paper
Correspondence Author:Zhou Wenxiao
Discipline:Science
First-Level Discipline:geology
Document Type:J
Volume:29
Issue:2
Page Number:280-294
ISSN No.:1674-487X
Translation or Not:no
Date of Publication:2018-04-17
Included Journals:SCI
Links to published journals:https://doi.org/10.1007/s12583-017-0942-2
Pre One : Geochronology and geochemistry of the Carboniferous Ulann Tolgoi granite complex from northern Inner Mongolia, China: Petrogenesis and tectonic implications for the Uliastai continental margin
Next One : Geochemistry and zircon geochronology of a gabbro-granodiorite complex in Tongxunlian, Inner Mongolia: partial melting of enriched lithosphere mantle
Date of Birth:1982-11-01
Date of Employment:2013-09-01
School/Department:综合地质研究中心
Education Level:Doctoral Degree in Education
Gender:Male
Degree:理学博士学位
Status:在岗
Discipline:mineral resource prospecting and exploration
tectonic geology
Geochemistry
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