Dongguashan Copper (gold) deposit i

Dongguashan Copper (gold) deposit is located in the
northeast of the Yangtze craton, which belong to the lower
Yangtze Syneclise Fanchang Guichi concave fault-fold
belt (Tang et al., 1998). It occurred in North East section
of Qingshan anticline, secondary structure of DatongShunan multiple syncline. The formation closely related to
mineralization including upper Devonaian Wutong
formation (D3w) quartz sandstone, middle-upper
Carboniferous Chuanshan and Huanglong formation (C2+3)
carbonate rock, lower Permian Qixia formation (P1q)
limestone, chert and skarn. The complex reticular
structure-framework in this area is compesed of NE
trending folds and faults of Indosinian and nearly SN-,
EW- and NNE trending faults, interlayer structure and
joint. Magmatic rock emplaced along the complex
structure systems, showed dykeand apophysis in shallow.
Qingshanjiao composite rock body is closely related to
mineralization, composed by granodiorite and
porphyraceous quartz monzodiorite.

結果 (中文) 1:

冬瓜山铜 （金） 矿床位于中东北的扬子克拉通，属于较低长江台繁昌贵池凹断层褶皱带 （唐 et al.，1998年）。它发生在东北地区部分青山背斜的二级结构的 DatongShunan 多向斜。的形成密切相关成矿作用包括上部 Devonaian 梧桐(D3w) 形成石英砂岩上部石炭系船山与黄龙的形成 (C2 + 3)碳酸盐岩下, 二叠统栖霞组 (P1q)石灰石、 硅质岩、 矽卡岩。复杂的网状在这一领域的结构框架是东北地区趋势的褶皱和断层的印支期和近 SN-，Ew 向和北北东向断裂、 夹层结构和联合。岩浆岩布设沿复杂结构系统，在浅表明 dykeand 隆起。分布着一复合岩体密切相关成矿作用，由花岗闪长岩和似石英组成。

結果 (中文) 3:

冬瓜山铜（金）矿床位于扬子克拉通的东北部，属于低长江向斜繁昌贵池凹褶断带（唐等，1998）。它发生在东北部青山背斜、向斜的次级结构的datongshunan多。密切相关的形成矿化包括上devonaian梧桐（d3w）形成的石英砂岩，中上部石炭系船山组、黄龙组（C2 + 3）碳酸盐岩，二叠系下统栖霞组（p1q）灰岩、硅质岩和矽卡岩型。复杂网状在这一领域的结构框架由NE向褶皱和断层的印支期和近SN—，东西向和北北东向断层、夹层结构和接缝。岩浆岩侵沿复杂结构系统，显示dykeand隆起浅。Qingshanjiao复合岩体密切相关由花岗闪长岩和成矿作用似斑状石英二。