Origin of Reverse Zoned Cr-Spinels from the Paleoproterozoic Yanmenguan Mafic-Ultramafic Complex in the North China Craton
Bai, Yang1,2; Su, Ben-Xun1,2; Xiao, Yan3; Lenaz, Davide4; Sakyi, Patrick Asamoah5; Liang, Zi2,3; Chen, Chen1,2; Yang, Sai-Hong3
刊名MINERALS
2018-02-01
卷号8期号:2
关键词compositional zoning spinel elemental exchange North China Craton
ISSN号2075-163X
DOI10.3390/min8020062
文献子类Review
英文摘要We conducted petrological and mineral chemistry investigations of Cr-spinel in ultramafic rocks of the Yanmenguan mafic-ultramafic complex in the North China Craton. The Cr-spinel grains occur as inclusions in enstatite, tschermakite, phlogopite, and olivine, or as interstitial grains among the aforementioned silicate minerals, and show concentric or asymmetrical textures. Back-scattered electron and elemental images and compositional profiles of the spinel grains indicate the presence of Cr- and Fe-rich cores and Al- and Mg-rich rims. The host silicate minerals display a decrease in Al and Mg contents accompanied by an increase in Cr and Fe away from the spinel. These textures and compositional variations suggest that subsolidus elemental exchange more likely gave rise to the compositional zonation, resulting in the transfer of Al and Mg from the silicate minerals to the spinel. The Mn, Ni, and Ti contents in spinel and the major elements of olivine-hosted spinel are relatively stable during subsolidus elemental diffusion and thus are more reliable tracers of primary high-temperature processes. The temperature estimates reveal that the subsolidus diffusion might have occurred at 600-720 degrees C, which could be linked to the regional metamorphic event.
WOS关键词HIGH-PRESSURE GRANULITES ; RHUM LAYERED INTRUSION ; MESOZOIC MINO TERRANE ; ALASKAN-TYPE COMPLEX ; IKI LAVA LAKE ; CHROME-SPINELS ; EASTERN DESERT ; CENTRAL JAPAN ; SANGGAN AREA ; PETROGENETIC INDICATOR
WOS研究方向Mineralogy ; Mining & Mineral Processing
语种英语
出版者MDPI
WOS记录号WOS:000427534300031
资助机构National Key R&D Program of China(2017YFC0601306) ; National Key R&D Program of China(2017YFC0601306) ; National Key R&D Program of China(2017YFC0601306) ; National Key R&D Program of China(2017YFC0601306) ; National Natural Science Foundation of China(41522203) ; National Natural Science Foundation of China(41522203) ; National Natural Science Foundation of China(41522203) ; National Natural Science Foundation of China(41522203) ; Youth Innovation Promotion Association, Chinese Academy of Sciences(2016067) ; Youth Innovation Promotion Association, Chinese Academy of Sciences(2016067) ; Youth Innovation Promotion Association, Chinese Academy of Sciences(2016067) ; Youth Innovation Promotion Association, Chinese Academy of Sciences(2016067) ; National Key R&D Program of China(2017YFC0601306) ; National Key R&D Program of China(2017YFC0601306) ; National Key R&D Program of China(2017YFC0601306) ; National Key R&D Program of China(2017YFC0601306) ; National Natural Science Foundation of China(41522203) ; National Natural Science Foundation of China(41522203) ; National Natural Science Foundation of China(41522203) ; National Natural Science Foundation of China(41522203) ; Youth Innovation Promotion Association, Chinese Academy of Sciences(2016067) ; Youth Innovation Promotion Association, Chinese Academy of Sciences(2016067) ; Youth Innovation Promotion Association, Chinese Academy of Sciences(2016067) ; Youth Innovation Promotion Association, Chinese Academy of Sciences(2016067) ; National Key R&D Program of China(2017YFC0601306) ; National Key R&D Program of China(2017YFC0601306) ; National Key R&D Program of China(2017YFC0601306) ; National Key R&D Program of China(2017YFC0601306) ; National Natural Science Foundation of China(41522203) ; National Natural Science Foundation of China(41522203) ; National Natural Science Foundation of China(41522203) ; National Natural Science Foundation of China(41522203) ; Youth Innovation Promotion Association, Chinese Academy of Sciences(2016067) ; Youth Innovation Promotion Association, Chinese Academy of Sciences(2016067) ; Youth Innovation Promotion Association, Chinese Academy of Sciences(2016067) ; Youth Innovation Promotion Association, Chinese Academy of Sciences(2016067) ; National Key R&D Program of China(2017YFC0601306) ; National Key R&D Program of China(2017YFC0601306) ; National Key R&D Program of China(2017YFC0601306) ; National Key R&D Program of China(2017YFC0601306) ; National Natural Science Foundation of China(41522203) ; National Natural Science Foundation of China(41522203) ; National Natural Science Foundation of China(41522203) ; National Natural Science Foundation of China(41522203) ; Youth Innovation Promotion Association, Chinese Academy of Sciences(2016067) ; Youth Innovation Promotion Association, Chinese Academy of Sciences(2016067) ; Youth Innovation Promotion Association, Chinese Academy of Sciences(2016067) ; Youth Innovation Promotion Association, Chinese Academy of Sciences(2016067)
内容类型期刊论文
源URL[http://ir.iggcas.ac.cn/handle/132A11/83034]  
专题中国科学院地质与地球物理研究所
通讯作者Bai, Yang; Sakyi, Patrick Asamoah
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, POB 9825, Beijing 100029, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, POB 9825, Beijing 100029, Peoples R China
4.Univ Trieste, Dept Math & Geosci, Via Weiss 8, I-34128 Trieste, Italy
5.Univ Ghana, Sch Phys & Math Sci, Dept Earth Sci, POB LG 58, Legon, Ghana
推荐引用方式
GB/T 7714
Bai, Yang,Su, Ben-Xun,Xiao, Yan,et al. Origin of Reverse Zoned Cr-Spinels from the Paleoproterozoic Yanmenguan Mafic-Ultramafic Complex in the North China Craton[J]. MINERALS,2018,8(2).
APA Bai, Yang.,Su, Ben-Xun.,Xiao, Yan.,Lenaz, Davide.,Sakyi, Patrick Asamoah.,...&Yang, Sai-Hong.(2018).Origin of Reverse Zoned Cr-Spinels from the Paleoproterozoic Yanmenguan Mafic-Ultramafic Complex in the North China Craton.MINERALS,8(2).
MLA Bai, Yang,et al."Origin of Reverse Zoned Cr-Spinels from the Paleoproterozoic Yanmenguan Mafic-Ultramafic Complex in the North China Craton".MINERALS 8.2(2018).
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