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tectonic hydrothermal fluids
相关语句
  构造热液
     There are various kinds of uranium source leading to the ore-formation of sandstone-type uranium deposits, it may come from rocks in the provenance areas, from uranium pre-enriched ore-hosting horizon themselves of the basin and from the uranium source underneath the basin (including uranium contained in the oilfield water and uranium introduced by tectonic hydrothermal fluids, etc.) .
     砂岩型铀矿成矿铀源的来源是多种多样的,可以是来自盆地周边的蚀源区岩石,也可以是盆地容矿层本身铀的预富集,还可以是来自盆地深部的铀源(包括油田水的铀、构造热液带出的铀等)。
短句来源
  相似匹配句对
     TECTONIC DYNAMICS OF FLUIDS AND ITS ADVANCE
     流体构造动力学及其研究现状与进展
短句来源
     HYDROTHERMAL FLUIDS AND GEOLOGICAL PROCESSES
     水热流体与地质作用
短句来源
     ON TECTONIC GENERATION AND HYDROTHERMAL ACTIVITY
     论构造序次与热液活动
短句来源
     (4) there were tensile faults in the upper crustal tectonic system for emplacement of magmatic hydrothermal fluids;
     (4)地壳上层构造体系中的张性断裂,以供岩浆热液的就位;
短句来源
     DISTRIBUTION AND TECTONIC ENVIRONMENTS OF THE HYDROTHERMAL FIELDS
     现代海底热液活动区的分布与构造环境分析
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According to research on tectonic basin formation and post tectonic deformation of the Devonian sedimentary, the geothermal events of tectonic hydrothermal fluid in the Devonian hydrothermal deposition basins in the Qinling orogen can be, roughly speaking, recognized as follows: 1 the geothermal event of the Devonian basin formation of extensional tectonism hydrothermal deposition (D 1); 2 the geothermal event of the end of the Late Devonian to the Carboniferous...

According to research on tectonic basin formation and post tectonic deformation of the Devonian sedimentary, the geothermal events of tectonic hydrothermal fluid in the Devonian hydrothermal deposition basins in the Qinling orogen can be, roughly speaking, recognized as follows: 1 the geothermal event of the Devonian basin formation of extensional tectonism hydrothermal deposition (D 1); 2 the geothermal event of the end of the Late Devonian to the Carboniferous extensional deformation of basin superimposing of deep source hot fluids(D 2);3 the geothermal event of compression deformation of basin superimposing of hydrothermal fluids in the Indo Chinese orogen(D 3);4 the geothermal event of nappe thrust deformation of the basin in the Early Yanshanian orogen and superimposing of deep source hydrothermal fluids and brittle deformation of the basin in the Late Yanshanian orogen (D 4); 5 the geoevent of brittle deformation of the basin in the Himalayan (D 5) In the coarse of sedimentary basin formation and evolution, geothermal regime is variable in the basin but still can be recovered on the basis of special approach In the recovery of geothermal state and geothermal evolution in the hydrothermal deposition basin, fluid inclusion of mineral, maturity grade of organism, thermometer of minerals and oxygen isotope can be employed to reconstruct paleo temperature of hydrothermal activities in the basin

根据对秦岭泥盆纪沉积盆地的构造成盆 -后期构造变形特征研究 ,秦岭造山带泥盆纪热水沉积成矿盆地中构造 -热流体地质事件可初步厘定如下 :1中泥盆世伸展构造成盆 -热水同生沉积成矿事件 (D1)。2晚泥盆世 -石炭纪伸展变形 -深源热流体叠加事件 (D2 )。3印支期挤压收缩变形 -热改造事件 (D3 )。 4燕山期逆冲推覆构造改造 -深源热流体叠加及脆性变形事件 (D4 )。 5喜玛拉雅山期脆性变形 (D5)。从盆地热状态及热演化研究角度看 ,盆地内充填地层体中有机质及矿物可以记录热状态及热演化历史 ,利用盆地内充填地层体中有机质及矿物温度计可以反演盆地内充填地层体形成时盆地热状态和盆地底部热流。认为热水沉积成矿盆地热状态及热演化主要研究方法有主要矿物流体包裹体测温、镜质体反射率 (R0 )法、氧同位素地质温度计法等。

Through the investigation on the characters of newly found orebody in the deep of Jinchuan Mining Areai.the author and his research group realized that the geological structure and hydrothermal fluid has played an important role in the formation of the rich orebody and massive orebody in the deep of Jinchuan deposit.It has been found that the mineralization and enrichment in deep reach of the Jinchuan mining area is not only related to the rock mass,but also closely associated with the spst minerogenetic...

Through the investigation on the characters of newly found orebody in the deep of Jinchuan Mining Areai.the author and his research group realized that the geological structure and hydrothermal fluid has played an important role in the formation of the rich orebody and massive orebody in the deep of Jinchuan deposit.It has been found that the mineralization and enrichment in deep reach of the Jinchuan mining area is not only related to the rock mass,but also closely associated with the spst minerogenetic tectonic hydrothermal fluid,the tectonic hydrothermal makes part of the primary minerogenetic materials active and reaccumulated at the low press and expanding portions of the fold or fault,and thus provides convincing evidence for seeking orebody in deep portions of the Jinchuan mining area.

笔者及其研究集体通过对金川深部发现新的工业矿体地质特征的研究 ,认识到了构造与热液流体对金川深部成富矿、特富矿的重要性。金川矿区深部矿化富集除与岩体有关外 ,还与成矿后的构造—热液关系密切 ,构造—热液使部分初始成矿物质产生活化 ,并在褶皱、断裂的低压扩容部位再次聚集。为今后金川深部找矿提供了有力依据

There are various kinds of uranium source leading to the ore-formation of sandstone-type uranium deposits, it may come from rocks in the provenance areas, from uranium pre-enriched ore-hosting horizon themselves of the basin and from the uranium source underneath the basin (including uranium contained in the oilfield water and uranium introduced by tectonic hydrothermal fluids, etc.). The paper focuses the discussion on the evaluation methods of the uranium source from provenance areas and ore-hosting...

There are various kinds of uranium source leading to the ore-formation of sandstone-type uranium deposits, it may come from rocks in the provenance areas, from uranium pre-enriched ore-hosting horizon themselves of the basin and from the uranium source underneath the basin (including uranium contained in the oilfield water and uranium introduced by tectonic hydrothermal fluids, etc.). The paper focuses the discussion on the evaluation methods of the uranium source from provenance areas and ore-hosting horizon, and oilfield water from the depth, which effect the ore-formation of sandstone-type uranium deposits.

砂岩型铀矿成矿铀源的来源是多种多样的,可以是来自盆地周边的蚀源区岩石,也可以是盆地容矿层本身铀的预富集,还可以是来自盆地深部的铀源(包括油田水的铀、构造热液带出的铀等)。重点对影响砂岩型铀矿成矿的蚀源区铀源、容矿层地层铀源及深部油田水铀源的评价方法进行了探讨。

 
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