Some Features of Fluid Inclusions in Garnets from the Seleteguole Skarn Cu-Mo Deposit, Jinghe County, Xinjiang, China
Some Features of Fluid Inclusions in Garnets from the Seleteguole Skarn Cu-Mo Deposit, Jinghe County, Xinjiang, China
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DOI：
10.1111/1755-6724.12374_74
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发表时间：
2014-12
影响因子：
3.3
通讯作者：
Wei Zhang;Xing-chun Zhang;Chengbiao Leng;W. Su
中科院分区：
文献类型：
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作者：
Wei Zhang;Xing-chun Zhang;Chengbiao Leng;W. Su
存款。浅棕红色石榴石以3-10 mm大小的浸染状斑点出现在白色角化长英质凝灰岩中，该凝灰岩与铜矿化花岗斑岩体直接接触。棕色石榴石以2-6 mm大小的四面体三八面体晶体的块状集合体形式出现在石榴石夕卡岩中，它靠近矿化的花岗斑岩体，有不规则的石英网脉和局部的白榴辉岩。黄绿色石榴石以3-5 mm大小的菱形十二面体晶体的集合体形式出现在相对较远的灰白色角长石粉砂岩中。
the deposit. Light brownish red garnet occurred as 3-10 mm sized disseminated spots in white hornfelsed felsic tuff which is directly in contact with the Cu-mineralized granite porphyry stock. Brown garnet occurred as massive aggregates of 2-6 mm sized tetragonal trisoctahedron crystals in the garnet skarn, which is close to the Cumineralized granite porphyry stock, with irregular quartz stockwork veins and local flaky molybdenite. Yellowish green garnet occurred as aggregates of 3-5 mm sized rhombic dodecahedron crystals in greyish white hornfelsed siltstone which is relatively far away from the