1) Baimianshi ore field
白面石矿田
2) Baiyin orefield
白银矿田
1.
A LA-ICP-MS U-Pb chronological study of zircons from meta-acidic volcanics in Baiyin orefield,Gansu Province: New evidence for metallogenic age of Baiyin type massive sulfide deposits;
甘肃白银矿田变酸性火山岩锆石LA-ICP-MS测年———白银式块状硫化物矿床形成时代新证据
2.
A LA-ICP-MS chronological study of basic volcanics in Baiyin orefield,Gansu,China
甘肃白银矿田基性火山岩的LA-ICP-MS同位素年代学
3) Tongshi gold field
铜石金矿田
1.
Tongshi gold field is located around Tongshi alkaline igneous sub-volcanic complex in the west Shandong province of China.
铜石金矿田位于鲁西中生代富碱次火山杂岩体———铜石岩体周围,该岩体侵入于燕山晚期,主要有闪长玢岩、二长斑岩和隐爆角砾岩组成。
2.
Tongshi gold field are mainly composed of cryptoexplosive rock type (Guilaizhuang type), stratified microdisseminated carbonate rock type (Mofanggou type), multiple scarn type, porphyry type and altered rock type deposits (spot); the major mineral is gold, companied with silver, cooper and iron mineralization which formed a completed ore-forming series.
铜石金矿田主要由隐爆角砾岩型 (归来庄式 )、碳酸盐岩层状微细浸染型 (磨坊沟式 )、夕卡岩叠加型、斑岩型和蚀变岩型等多种类型的矿床 (点 )组成 ,矿种以金为主 ,伴有银、铜、铁矿化 ,构成一个较完整的成矿亚系列。
3.
In this paper, the analysis is made of the comprehensive information features of the gold-forming geological background of the Tongshi gold field; then a detailed investigation is presented into the component znation tr.
地质异常单元圈定矿产资源体潜在地段是以地质异常矿体定位理论为前提，应用综合信息定量标度“致矿地质异常单元”首先分析了铜石金矿田金矿成矿地质背景的综合信息特征，详细研究了“致矿地质异常”的组分分带趋势；推断了金矿产资源体系列形成的深部地质结构样式；在此基础上，选择控矿地质异常标志和地质矿异常标志作为构置成矿有利度的变量，利用成矿有利度圈定矿产资源体潜在地段。
4) Baiyin Mining Field
白银厂矿田
1.
Tectonic significance and origin of the rhyolites from Baiyin Mining Field in Gansu Province;
甘肃白银厂矿田流纹岩的成因及其构造意义
5) Baiyinchang orefield
白银厂矿田
1.
This paper deals with the occurrences, typomorphic characteristics and the main petrological parameters of the zircons in the deferent rocks of the Baiyinchang orefield, by Pupin′s study method on the zircon genesis mineralogy in detail.
Ｐｕｐｉｎ的锆石成因矿物学研究方法，详细研究了甘肃白银厂矿田各类岩石的锆石产出状态、晶体的标型特征及主要岩石学参数。
2.
The Baiyinchang orefield is a typical bigger massive sulfide polymetallic orefield, which located on the eastern part of the Qilian mountain chains.
甘肃白银厂矿田地处北祁连山东部，是一个典型的规模较大的块状硫化物多金属矿田。
6) Baishigou minefield
白石沟井田
1.
The Baishigou minefield is a larger medium minefield demonstrated in recent years,it locates at eastern south limb of Wuzhiling-Baizhai anticline,on a graben between Gangyayao and Liangshan faults,basic structural form is a broad and gentle anticline plunging east.
白石沟井田是近年来探明的大中型井田,位于五指岭—白寨背斜东端之南翼,新密—新郑复向斜之北翼,岗亚腰断层和梁山断层之间的地垒构造上,其基本构造形态为一向东倾伏的宽缓背斜。
补充资料：白面瑶寨
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说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条