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tectonic altered
相关语句
  构造蚀变
     The primary gold includes gold bearing quartz vein type,associated gold type,tectonic altered rock type,magma type and dissemination type.
     原生金矿有含Au石英脉型、伴生金型、构造蚀变岩型、岩浆岩型及浸染型。
短句来源
     The Hanshan gold deposit is a tectonic altered rock type deposit discovered recently in North Qilian Mountains.
     寒山大型金矿是近年来在北祁连山西段发现的与侵入岩有关的构造蚀变岩型金矿。
     Accordingly,the emphasis must by placed on the prospecting of tough shear zone type and tectonic altered rock type gold deposits.
     因此 ,在库斯拉甫地区 ,应注重寻找韧性剪切带型金矿和构造蚀变岩型金矿。
短句来源
     THE CHARACTERISTICS OF THE WALL ROCK AND HOST ROCK OF THE ORTHOPHYRIC TECTONIC ALTERED ROCK TYPE GOLD DEPOSITS IN QIANHE AREA
     前河地区正长斑岩构造蚀变岩型金矿围岩及容矿岩石特征
短句来源
     THE CHARACTERISTICS OF THE GOLD DEPOSITS OF TECTONIC ALTERED ROCK TYPE IN THE OPHIOLOTE OF NORTH AILAO MOUNTAIN
     哀牢山北段蛇绿岩中构造蚀变岩型金矿床特征
短句来源
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  “tectonic altered”译为未确定词的双语例句
     18 orebody is the type of the porphyry gold deposit,going with the orthophyric tectonic altered rock-type Using the mapping of the alteration , magnetization, morphology and chemical typomorphic of pyrite , Preliminary studies suggest that there are unknown rich ore segment under -400m deep . So the bottom of the drillings of ZK18-4 should be explored especially.
     据热液蚀变、磁化率、黄铁矿形态及化学成分标型的矿物学填图,认为“18号矿体”-400m以下在ZK18-4号孔金矿化较强,尤其应加强对ZK18-4孔及其邻区深部的勘查。
短句来源
     The gold deposits of quartz vein type and tectonic altered rock type are controlled respectively by NE and NWW second faults, the porphyry explosion breccia type gold deposits are tightly related with the Yanshanian shallow or ultra shallow intrusive (explosive) granite porphyry.
     区内石英脉型金矿主要受北东向次级断裂控制 ,破碎带蚀变岩型金矿受北西西向次级断裂控制 ,斑岩—爆破角砾岩型金矿与燕山期浅成—超浅成侵入 (爆破 )花岗斑岩关系密切。
短句来源
  相似匹配句对
     and tectonic movement.
     (3)与深部地质作用有关;
短句来源
     ON TECTONIC SYSTEMS
     论构造体系
短句来源
     THE CHARACTERISTICS OF THE GOLD DEPOSITS OF TECTONIC ALTERED ROCK TYPE IN THE OPHIOLOTE OF NORTH AILAO MOUNTAIN
     哀牢山北段蛇绿岩中构造蚀变岩型金矿床特征
短句来源
     On Diameters of Altered Graphs
     变更图的直径(英文)
短句来源
     It is considered that it belongs to the gold field of the tectonic altered rock type which is relative to the metamorphic-hydrothermal solution.
     初步认为矿床类型属于与变质热液有关的构造蚀变岩型金矿床。
短句来源
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The Jiaojia gold deposit, an important special type of gold deposit in China, occurs in a fracture zone. Tectonite has undergone intense alteration. Widespread potash feldspathization is considered to be the metallogenic indicator, but gold is concentrated in a pyrite-sercitized tectonite zone. Based on a study of the geological features of the deposit, features of tectonic altered rocks, trace elements in altered rocks and stable isotopes and mineral inclusions of the deposit, this paper discusses...

The Jiaojia gold deposit, an important special type of gold deposit in China, occurs in a fracture zone. Tectonite has undergone intense alteration. Widespread potash feldspathization is considered to be the metallogenic indicator, but gold is concentrated in a pyrite-sercitized tectonite zone. Based on a study of the geological features of the deposit, features of tectonic altered rocks, trace elements in altered rocks and stable isotopes and mineral inclusions of the deposit, this paper discusses the genesis and ore-forming physico-chemieal conditions of the Jiaojia gold deposit. The ore-forming temperature is 310℃, the pressure is about 800×10~5Pa, oxygen fugacity fo_2=10~(-34) to 10~(-36), the ore-forming solutions are rich in K~(1+) and Cl~(1-) ions. It is suggested that the upper Archean—Lower Proterozoic Jiaodong Group is the Au-bearing formation, which served as it gold source. The formation of the Jiaojia gold deposit is related to the Yanshanian faulting and anatexis of the Shangzhuang granodiorite. The deposit is a mesothermal gold deposit.

焦家金矿明显受断裂破碎带控制,围岩蚀变强烈,是我国特有的重要金矿类型。本文通过矿床地质特征、矿物中流体包裹体和稳定同位素研究确定焦家金矿成矿温度为310℃,压力800×10~5pa,fo_2为10~(-34)—10~(-36)。成矿溶液为富钾、氯的流体。金来自胶东群含金建造,成矿与尚庄花岗闪长岩有关,为中深,中温岩浆热液金矿床。

The gold deposits of tectonic altered rock type in the ophiolite of Noith Ailao Mountain are located in the basalts and pyroclastic rocks of the upper ophiolite. The gold deposits are all under the control of northwest faulted structure, and associated with the different veins of lamprophyres and granodioritic porphyrys which have to do with ore-forming process. First wall-rock alteration is carbonation, second are sericitization and pyritisation. Main metallic sulphide ores are pyrites, arsenopyrites,...

The gold deposits of tectonic altered rock type in the ophiolite of Noith Ailao Mountain are located in the basalts and pyroclastic rocks of the upper ophiolite. The gold deposits are all under the control of northwest faulted structure, and associated with the different veins of lamprophyres and granodioritic porphyrys which have to do with ore-forming process. First wall-rock alteration is carbonation, second are sericitization and pyritisation. Main metallic sulphide ores are pyrites, arsenopyrites, stibnites, and form the different assemblages of min-eralization. The forming temperature of the gold deposits is low- to -moderate. The compo-sition of the fluid inclusions is abundant in Na+, Zn2+, Cl-; SO42- , H2O, CO2and so on. The main enrichmicroelements of the gold deposits are As, Sb, W, and REE evolutionary charac-teristics are LREE depressing and HREE increasing. Sulfur and oxygen isotope composition displays that the gold deposits are low -to -moderate hydrothermal deposits and their ore -forming solution is mainly composed of the magmatic hydrothermal solution which is added in some underground water.

哀牢山北段蛇绿岩中构造蚀变岩型金矿床主要产于蛇绿岩上部的玄武岩和火山碎屑岩中,并受北西向断裂构造控制。区内分布有喜玛拉雅期煌斑岩和花岗闪长斑岩等脉岩,其与成矿作用密切相关。围岩蚀变以碳酸盐化为主,其次是绢云母化和黄铁矿化。矿石主要金属矿物为黄铁矿、毒砂、辉锑矿;包裹体成分以Na~+、Zn~(2+)、Cl~-、SO_4~(2-)、H_2O和CO_2为主;主要微量元素是As、Sb、W;稀土元素表现出轻稀土降低和重稀土相对增加的演化特征。硫、氧同位素研究表明,该矿床属于以岩浆热液为主,伴有部分地下水加入的中低温热液矿床。

Dense Au deposit zone is located in the suture between Archaeozoic Zhongchao ancient land plate and Proterozoic Mongoliasea plate , controlled by NW Fuerhe and Gudonghe lithosphericfractures. Au ores are generally enriched in the edges of abovementioned plates, intermediate-acid intrusive complex related to ore-forming resulted from anatectic granite magma. Hoststructures are usually ductile shearzones or schistosity zones in brittle fracture zones. Au ores dominantly belong to sulphide-lacked type, and then...

Dense Au deposit zone is located in the suture between Archaeozoic Zhongchao ancient land plate and Proterozoic Mongoliasea plate , controlled by NW Fuerhe and Gudonghe lithosphericfractures. Au ores are generally enriched in the edges of abovementioned plates, intermediate-acid intrusive complex related to ore-forming resulted from anatectic granite magma. Hoststructures are usually ductile shearzones or schistosity zones in brittle fracture zones. Au ores dominantly belong to sulphide-lacked type, and then to tectonic altered rock type. The dense Au ore zone possesses excellent metallogenic conditions, is the mainprospect area of Au deposits in Jilin Province.

金矿密集带位于太古宙中朝古陆板块与元古宙蒙古海板块之间的缝合线上,受北西向的富尔河-古洞河岩石圈断裂带控制。金矿床普遍产在上述相邻二板块构造的边缘,与成矿有关的中酸性侵入杂岩体多为深熔花岗岩浆的产物,容矿构造往往为韧性剪切带或脆性构造破碎带内的片理化带。金矿床主要为少硫化物型,次为构造蚀变岩型,该带有优异的成矿条件,是吉林省金矿的主要远景区。

 
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