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Characteristics and dynamic settings of the Central-east Asia multi-energy minerals metallogenetic domain 被引量:13
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作者 LIU ChiYang QIU XinWei +1 位作者 WU BoLin ZHAO HongGe 《Science China Earth Sciences》 SCIE EI CAS 2007年第z2期1-18,共18页
That more than 82 percent of proved sandstone-type uranium deposits coexist with proved oil-gas or coalfields in the world reflects the fact of coexistence and accumulation of multi-energy minerals including oil,gas,c... That more than 82 percent of proved sandstone-type uranium deposits coexist with proved oil-gas or coalfields in the world reflects the fact of coexistence and accumulation of multi-energy minerals including oil,gas,coal and uranium in the same basin.Especially,this phenomenon is most typical in the Central-east Asia energy basins.Across China,Mongolia and some central Asian countries,the giant Central-east Asia metallogenetic domain(CEAMD)stretches more than 6,000 km from Songliao Basin of China in the east to the Caspian Sea in the west.The multi-energy minerals distribution characteristics of the domain include:their spatial distribution is complicated and ordered;the ore-bearing horizon relates closely to the geographical region;the accumulation/mineralization and localization time is the same or close;the occurrence setting and accumulation/mineralization have close correlation;and they have rich provenance for all the minerals.All of these imply that they have close relations between each other under a unified geodynamic background.The exogenetic uranium mineralization process in CEAMD can be divided into five phases using time limits of 100 Ma,(50±2)Ma,20±(2―4)Ma,8―5 Ma.The major mineralization periods and their differences in each primary uranium-bearing basin are identical to the oil-gas accumulation and localization periods and phases in the same basin,and are also in response to regional tectonics and controlled in general by the regional geodynamic environment.For industrial application and commercial exploitation,it is suggested that an important period for coexistence,accumulation and localization of oil,gas,coal and uranium and their interaction mainly occur in the late/last and post basin evolution.Through generalized analysis and comparison of accumulation/mineralization environment of the energy basins in CEAMD,the authors propose that the relatively stable regional tectonic background and moderate(weaker)structural deformation probably are necessary for formation,coexistence and preservat 展开更多
关键词 Central-east Asia energy minerals metallogenetic domain oil-gas-coal and sandstone-type uranium ore deposit coexistence in the same basin accumulation/mineralization mechanism basin dynamics
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多种能源矿产赋存与盆地成藏(矿)系统 被引量:77
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作者 刘池洋 赵红格 +1 位作者 谭成仟 王建强 《石油与天然气地质》 EI CAS CSCD 北大核心 2006年第2期131-142,共12页
沉积盆地是诸多沉积矿产成生、赋存的基本单元和成藏(矿)的大系统,具有既相对独立又统一的成藏(矿)环境和动力学背景,有其自身的成矿特点和规律,可命名为盆地成藏(矿)系统(单元)以与造山带等成矿系统相并列和区别。目前国内外的矿产勘... 沉积盆地是诸多沉积矿产成生、赋存的基本单元和成藏(矿)的大系统,具有既相对独立又统一的成藏(矿)环境和动力学背景,有其自身的成矿特点和规律,可命名为盆地成藏(矿)系统(单元)以与造山带等成矿系统相并列和区别。目前国内外的矿产勘查、开采利用和研究揭示,油、气、煤和铀主要赋存在沉积盆地中。这4种重要能源矿产同盆共存富集存在普遍、含矿层位联系密切、空间分布复杂有序、赋存环境和成藏(矿)作用有机相关、成藏(矿)-定位时期相同或相近,表明其间有着密切的内在联系和统一的地球动力学背景。在盆地演化和后期改造过程中,油、气、煤、铀等沉积矿产同盆成生共存、相互作用、各自成藏(矿)和改造定位。它们成生-成藏(矿)和定位的主要期次,与盆地演化-改造的阶段及主要地质事件有明显的响应联系和密切的耦合关系。文中讨论了其中部分相关前沿科学问题,初步建立了鄂尔多斯盆地演化-改造阶段及其主要地质事件与油、气、煤、铀成藏(矿)作用期次的时序对应关系。 展开更多
关键词 油-气-煤-砂岩铀矿 同盆共存 成藏(矿)机理 盆地动力学 盆地成藏(矿)系统 多种能源 鄂尔多斯盆地
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The radioactive abnormality characteristics of typical regions in Ordos Basin and its geological implications 被引量:6
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作者 TAN ChengQian LIU ChiYang ZHAO JunLong ZHANG RongRong 《Science China Earth Sciences》 SCIE EI CAS 2007年第z2期174-184,共11页
There are many results of single mineral enrichment characteristic, such as oil, gas, coal and uranium, but little is known about the synergistic research of these important minerals and the study of uranium enrichmen... There are many results of single mineral enrichment characteristic, such as oil, gas, coal and uranium, but little is known about the synergistic research of these important minerals and the study of uranium enrichment features in the deep basin. So, the study on the paragenesis regularity and coexisting relation of many minerals in the basin will promote the integrated forecast and cooperative exploitation of the basin. Based on the plentiful logging data and geological data, this paper studies the distributing feature of higher Gamma abnormality. The analysis on 33 core samples' test results indicates that the increasing of Gamma abnormality is due to the increasing of the uranium element, and the enrichment of uranium is a result of the activation and conglomeration of uranium. On the basis of the recognization of radioactive abnormality and the study about the reality of oil,gas,coal or uranium coexisting in a basin and its mechanism, the paper shows that there is a certain mutual promotion in oil, gas, coal and uranium in the basin, which provides an important theory basis for cooperative exploitation of energy resources. 展开更多
关键词 ORDOS basin RADIOACTIVE abnormality test analysis oil-gas-coal-uranium coexisting PARAGENESIS
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亚洲东部碰撞构造:郯庐—尚塔尔碰撞带研究 被引量:1
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作者 张培强 马宇 《地质找矿论丛》 CAS CSCD 2006年第3期203-209,共7页
沿郯城—庐江断裂带两侧各约500 km内发育的中生代以来白云母花岗岩、二云母花岗岩和A型花岗岩,五大连池、科洛和二克山火山岩带的强碱性富钾火山岩,高87Sr/86Sr值、低εNd值的中新生代玄武岩,沿郯庐断裂带两侧盆地广泛发育的磨拉石建造... 沿郯城—庐江断裂带两侧各约500 km内发育的中生代以来白云母花岗岩、二云母花岗岩和A型花岗岩,五大连池、科洛和二克山火山岩带的强碱性富钾火山岩,高87Sr/86Sr值、低εNd值的中新生代玄武岩,沿郯庐断裂带两侧盆地广泛发育的磨拉石建造,稀土元素∑REE,∑LREE,∑LREE/∑HREE从老到新均逐渐增高;郯庐断裂带莫霍面深度明显大于两侧盆地;郯庐断裂带两侧地块的不连续与差异;沿郯城—庐江断裂带展布的华北地台北缘及东缘的高压麻粒岩、NNE向展布的日照、莒南、东海榴辉岩超高压带和安徽张八岭高压蓝片岩带;郯庐断裂带内表现的强烈挤压构造;郯庐断裂带东侧胶辽—苏北黄海负磁异常区不同于周围地质体(正磁异常区)等,所有证据都指示着南起安徽庐江,经山东郯城、黑龙江佳木斯,北至俄罗斯尚塔尔群岛的断裂带及其两侧构造带为一构造碰撞带:郯庐—尚塔尔碰撞带,郯庐—尚塔尔断裂带为碰撞带的缝合线。松辽盆地、华北盆地、苏北盆地等成煤、成油气等矿产的盆地是碰撞的结果。碰撞带的(突出)应力集中区鲁西—胶东超高压带碰撞区、燕山—辽东碰撞区是中国东部地震的高发区。碰撞的主要动力机制为日本海和鄂霍次克海的张开及菲律宾板块的俯冲。 展开更多
关键词 郯庐-尚塔尔碰撞带 油-气-煤盆地 地震 渤海湾形成
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煤油气共生矿井采煤工作面底板卸压变形规律研究及应用
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作者 李川 《煤矿安全》 CAS 北大核心 2019年第9期228-231,共4页
通过黄陵二号煤矿203采煤工作面底板卸压和底板钻孔孔壁变形情况观测,以及对钻孔内瓦斯浓度和瓦斯压力变化情况的检测,开展了采煤工作面底板卸压变形规律研究。研究结果表明,工作面推进至距底板钻孔约10 m时,底板卸压并开始发育裂隙;随... 通过黄陵二号煤矿203采煤工作面底板卸压和底板钻孔孔壁变形情况观测,以及对钻孔内瓦斯浓度和瓦斯压力变化情况的检测,开展了采煤工作面底板卸压变形规律研究。研究结果表明,工作面推进至距底板钻孔约10 m时,底板卸压并开始发育裂隙;随着采煤工作面推过底板钻孔后,逐渐远离底板钻孔,底板卸压范围逐渐向底板深部扩大,测点位置钻孔变形和破坏越来越严重。采空区后方10~30 m范围内,工作面底板下10~30 m,出现最大卸压变形以及瓦斯(油型气)的大量涌出。据此优化了205采煤工作面底板煤层及油气层瓦斯抽采技术参数。 展开更多
关键词 瓦斯抽采 采煤工作面 煤油气共生 底板卸压 变形规律
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