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- W3140052698 abstract "在上最近三十年，在 Huanggangliang 的大尺寸的 Sn-Fe polymetallic 矿石存款的探索， Da Hinggan 山，内部蒙古，中国，大部分集中于矿化作用代表的前提 epigenetic magmatic 在有中生代 magmatism 的基因连接的热水的矿石沉积物。Huanggangliang Sn-Fe polymetallic 矿石存款发生在二叠的阶层，与 Zhesi 形成的 siltstone/marble 和 Dashizhai 形成的 spilite/andesite/tuff。特征地质并且 geochemical 数据证明那个沉积热水的矿化作用发生在盆进化期间在二叠，而非代表 epigenetic magmatic 有下列证据的热水的开始。忍受矿石的 skarns 与内在的 metasedimentary 岩石和 overlying 是层状的暴烈的沉积岩石。沉积热水的质地和结构在 stratabound 被观察忍受矿石的 skarn 象有小尺寸的合拢或软变丑， skarn 的 synsedimentary 角砾岩和磁铁矿矿石和磁铁矿矿石的同心的壳结构的把床压成薄片的 skarn 和磁铁矿矿石那样。那么忍受矿石的 skarns 与磁铁矿矿石和微传播锡联系了的 stratabound，是 exhalite 的古怪例子。stratabound 的 REE 内容忍受矿石的 skarns 显示 LREE 富有(36.91" @default.
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- W3140052698 date "2010-01-01" @default.
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- W3140052698 title "Geology and geochemistry of Huanggangliang stratabound skarn deposit in Inner Mongolia, China" @default.
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