1) fenfangwanliang gold deposit
粉坊湾梁金矿
1.
The fenfangwanliang gold deposit is located in west part of fault depression belt with east|west direction between Liuba in Shanxi province and Huixian Dahedian in Gansu province, which is distruted in Mid|Qinling Mountain Au|Hg deposit belt.
粉坊湾梁金矿位于陕西留坝至甘肃徽县大河店东西向断陷带西段,中秦岭金汞成矿带上,矿床受构造及特殊地层控制,含火山凝灰质的岩层是成矿的物质基础,岩浆活动及期后热液活动对成矿也起着极为重要的作用,找矿标志突出,根据矿床分布规律,可确定找矿方向。
2) Dianfang gold deposit
店坊金矿
1.
Dianfang gold deposit is located at the east part of the Machaoying fault zone, andhosting in the south contact of an explosive breccia chimney, Xionger Group.
店坊金矿产在中元古代熊耳群爆破角砾岩体的南部，与马超营断裂带东延部分有关。
3) Mofanggou gold deposit
磨坊沟金矿
1.
Fluid inclusions of Mofanggou gold deposit are tested and studied.
对磨坊沟金矿床流体包裹体进行了测试研究 ,结果表明主要成矿阶段的温度为 1 2 0～360℃ ,包裹体盐度在 0 。
4) Laowan gold deposit
老湾金矿
1.
The Laowan gold deposit in Henan Province,one of the most important gold deposits in the Qinling-Dabie orogenic belt,is hosted within Proterozoic metamorphic rocks,controlled by the Lanwan NWW-trending shear zone and related to the nearby Laowan Yanshanian granite.
河南老湾金矿是秦岭—大别造山带中代表性金矿之一,其容矿围岩是元古宙变质岩,矿体受到NWW向老湾剪切带的控制,同时附近又有燕山期花岗岩。
2.
The Laowan gold ore belt is an important component part of the Tongbai-Dabieshan(northern slope) gold-silver metallogenic belt,and the Laowan gold deposit is one of the major deposits in this belt and also one of the important large-size metamorphic clastic rock gold deposits in China.
老湾金矿带是桐柏—大别山(北坡)金银成矿带的重要组成部分,老湾金矿床是该成矿带的主要矿床之一,同时也是我国重要的变质碎屑岩型大型金矿之一。
3.
The materias source base and material condition of mineralization, the main source of rare earths element in ore of Laowan Gold Deposit are analyzed.
分析了老湾金矿成矿的物源基础、成矿的物质条件和矿石中稀土元素的主要来源;论述了矿床中硫同位素组成不平衡的原因:通过老湾金矿床矿石铅同位素和成矿流体的研究,发现老湾金矿床成矿物质主要来自有热水沉积作用的中元古界龟山岩组地层,少部分来自老湾花岗岩体。
5) Aiwan gold deposit
崖湾金矿
1.
Aiwan gold deposit is located in the middle part of Lintan—Lixian—Zhashui geosynline zone.
崖湾金矿位于秦岭活动带礼县—柞水被动陆缘带中段。
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