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首页> 外文期刊>Geoscience frontiers >Tourmaline from the Archean G.R.Halli gold deposit, Chitradurga greenstone belt, Dharwar craton (India): Implications for the gold metallogeny
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Tourmaline from the Archean G.R.Halli gold deposit, Chitradurga greenstone belt, Dharwar craton (India): Implications for the gold metallogeny

机译:来自Dharwar克拉通(印度)的Archean G.R. Halli金矿的电气石,Chitradurga绿岩带,印度的金矿成矿作用

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Tourmaline occurs as a minor but important mineral in the alteration zone of the Archean orogenic gold deposit of Guddadarangavanahalli (G.R.Halli) in the Chitradurga greenstone belt of the western Dharwar craton, southern India. It occurs in the distal alteration halo of the G.R.Halli gold deposit as (a) clusters of very fine grained aggregates which form a minor constituent in the matrix of the altered metabasalt (AMB tourmaline) and (b) in quartz-carbonate veins (vein tourmaline). The vein tourmaline, based upon the association of specific carbonate minerals, is further grouped as (i) albite-tourmaline-ankerite-quartz veins (vein-1 tourmaline) and (ii) albite-tourmaline-calcite-quartz veins (vein-2 tourmaline). Both the AMB tourmaline and the vein tourmalines (vein-1 and vein-2) belong to the alkali group and are classified under schorl-dravite series. Tourmalines occurring in the veins are zoned while the AMB tourmalines are unzoned. Mineral chemistry and discrimination diagrams reveal that cores and rims of the vein tourmalines are distinctly different. Core composition of the vein tourmalines is similar to the composition of the AMB tourmaline. The formation of the AMB tourmaline and cores of the vein tourmalines are proposed to be related to the regional D 1 deformational event associated with the emplacement of the adjoining ca. 2.61?Ga Chitradurga granite whilst rims of the vein tourmalines vis-à-vis gold mineralization is spatially linked to the juvenile magmatic accretion (2.56–2.50?Ga) east of the studied area in the western part of the eastern Dharwar craton. Graphical abstract Display Omitted Highlights ? Tourmaline occurs in the distal wall rock alteration halo of the Neoarchean G.R.Halli gold deposit, Dharwar craton, India. ? It belongs to the alkali group and classifies under schorl-dravite series. ? Core and rim chemistry of these tourmalines are related with two different geological events.
机译:电气石是印度南部达哈尔克拉通的奇特拉杜尔加绿岩带古达达拉格万哈哈里(G.R. Halli)太古宙造山金矿床蚀变带中的一种次要但重要的矿物。它发生在GRHalli金矿床的远端蚀变晕中,是因为(a)非常细粒的聚集体簇,在改变的玄武岩(AMB电气石)的基质中形成次要成分,并且(b)在石英碳酸盐岩脉(静脉)中电气石)。基于特定碳酸盐矿物的缔合,电气石电气石又可分为(i)钠长石-电气石-方铁矿-石英脉(静脉1电气石)和(ii)钠长石-电气石-方解石-石英脉(静脉2电气石)。 AMB电气石和静脉电气石(静脉1和静脉2)均属于碱性基团,并被分类为schorl-dravite系列。发生在静脉中的电气石被划分区域,而AMB电气石未被划分区域。矿物化学和鉴别图表明,静脉电气石的核心和边缘明显不同。静脉电气石的核心成分类似于AMB电气石的成分。 AMB电气石的形成和静脉电气石的核心被认为与区域D 1变形事件有关,该事件与相邻ca的位置有关。 2.61?Ga Chitradurga花岗岩,脉状电气石的边缘相对于金矿化,在空间上与东部Dharwar克拉通的研究区域以东的岩浆增生(2.56-2.50?Ga)有关。图形摘要显示省略的突出显示?电气石发生在印度Dharwar克拉通的Neoarchean G.R. Halli金矿的远端围岩蚀变晕中。 ?它属于碱族,属于schorl-dravite系列。 ?这些电气石的核心和边缘化学与两个不同的地质事件有关。

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