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 |
DOI | 10.3390/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/132A11/83032] |
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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