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少砬哈子碱性岩体铌钽矿化特征及吉中地区碱性岩找矿方向 被引量:1
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作者 陈刚 赵娟 +3 位作者 翟玉春 张星 徐海军 崔天夫 《吉林地质》 2011年第4期36-39,共4页
在吉中地区敦密断裂带上,分布大小不等的碱性杂岩体已发现的大约20余个。本文对蛟河南部少砬哈子碱性岩体地质特征及蚀变矿化进行了详细的野外地质调查,发现该岩体具有很好的铌、铈矿化,Nb5O2平均品位0.043%,最高为0.049%(未分析钽),铈... 在吉中地区敦密断裂带上,分布大小不等的碱性杂岩体已发现的大约20余个。本文对蛟河南部少砬哈子碱性岩体地质特征及蚀变矿化进行了详细的野外地质调查,发现该岩体具有很好的铌、铈矿化,Nb5O2平均品位0.043%,最高为0.049%(未分析钽),铈族稀土质量分数0.109%,且不同的岩相带矿化蚀变存在较大差异,细粒结构相矿化相对较好;通过电镜扫描,确定了含铌钽的矿物为褐钇铌矿,为选矿提供了依据;结合区域成矿地质条件分析,认为分布在吉中地区敦密断裂带上的这些碱性杂岩是寻找稀有元素矿产的重要靶区。 展开更多
关键词 粗面岩 敦密断裂带 铌矿 吉中地区
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关于吉中地区大河深组的含义及其时代的商榷 被引量:2
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作者 曹云龙 贾洪波 +1 位作者 吕新宇 颜世凯 《吉林地质》 2012年第1期1-3,11,共4页
大河深组主要分布在吉林中部,本文从岩性、时代、生物组合对分布于二叠系寿山沟组之上的中酸性火山岩、火山碎屑岩夹少量的沉积岩进行了分析及对比,阐明了其作为大河深组的意义。
关键词 吉中地区 早二叠世 大河深 对比 中、酸性火山岩
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吉中地区下二叠统大河深岩组岩石学特征及锆石U-Pb年代学研究 被引量:1
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作者 赵大印 王迪 《吉林地质》 2022年第1期12-18,共7页
本文通过对吉中地区下二叠统大河深岩组地质剖面的测制及LA-ICP-MS锆石U-Pb年代学研究,对其岩石学特征及成岩时代进行了探讨。研究表明,大河深岩组为一套中酸性火山岩组合,并夹少量粉砂岩;其变流纹岩锆石U-Pb加权平均年龄值为296.5±... 本文通过对吉中地区下二叠统大河深岩组地质剖面的测制及LA-ICP-MS锆石U-Pb年代学研究,对其岩石学特征及成岩时代进行了探讨。研究表明,大河深岩组为一套中酸性火山岩组合,并夹少量粉砂岩;其变流纹岩锆石U-Pb加权平均年龄值为296.5±2.2 Ma(MSWD=2.3,n=16),该年龄可以代表大河深岩组的形成年龄,时代为早二叠世。 展开更多
关键词 吉中地区 大河深岩组 地层
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《吉中地区构造格架与地壳演化》研究的新进展 被引量:1
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作者 彭玉鲸 苏养正 《吉林地质科技情报》 1996年第2期3-9,共7页
关键词 吉中地区 构造格架 地壳演化
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吉林中部地区二叠纪岩相古地理及沉积构造背景 被引量:16
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作者 杨宝忠 夏文臣 杨坤光 《现代地质》 CAS CSCD 北大核心 2006年第1期61-68,共8页
以沉积体系研究为基础,综合应用沉积岩碎屑物质成分统计、岩石地球化学分析等方法,详细地研究了吉林中部地区二叠纪沉积特征。结合沉积构造背景分析,重建吉林中部地区二叠纪岩相古地理及构造古地理。研究发现:早—中二叠世吉林中部地区... 以沉积体系研究为基础,综合应用沉积岩碎屑物质成分统计、岩石地球化学分析等方法,详细地研究了吉林中部地区二叠纪沉积特征。结合沉积构造背景分析,重建吉林中部地区二叠纪岩相古地理及构造古地理。研究发现:早—中二叠世吉林中部地区具活动大陆边缘的复合边缘海盆特征,早二叠世发育了碳酸盐岩陆架、陆架边缘沉积体系及(次)深水盆地沉积体系,相序具有向上变浅的旋回特征;中二叠世初期,地壳活动强烈,火山发育,其后沉积了盆缘冲积扇沉积体系、(次)深水盆地沉积体系以及向上变浅的碳酸盐缓坡沉积体系等;晚二叠世东北中、小板块群与华北板块沿西拉木伦河—长春—延吉缝合带拼合,古地理发生重大变化,整个地区由海相环境转为陆相环境,仅局部地区有残留的海水,发育了湖缘冲积扇、次深湖沉积体系。 展开更多
关键词 二叠纪 沉积体系 吉中地区 沉积相 构造背景
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吉林省中部地区西别河组层序
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作者 刘慧 《石油石化物资采购》 2019年第9期70-70,25,共2页
吉中地区晚志留-早泥盆世地层(西别河组)仅出露于永吉县的张家屯、小绥河和二道沟等地,原称为张家屯组、二道沟组和小绥河组,地层层序自下而上究竟是张家屯组-小绥河组-二道沟组还是张家屯组-二道沟组-小绥河组,一直存在异议。本次研究... 吉中地区晚志留-早泥盆世地层(西别河组)仅出露于永吉县的张家屯、小绥河和二道沟等地,原称为张家屯组、二道沟组和小绥河组,地层层序自下而上究竟是张家屯组-小绥河组-二道沟组还是张家屯组-二道沟组-小绥河组,一直存在异议。本次研究重新测制了二道沟组、小绥河组剖面。首次在小绥河组中发现指示顶底关系的珊瑚礁,珊瑚礁正常生长,说明当前地层未发生倒转,为正常层序;其次,在小绥河组中发现负载构造(卷曲层理),砂层沉积陷入到饱含水的塑性泥层上,砂层在上,泥层在下,也说明层序正常。另外将张家屯组、二道沟组和小绥河组与黑龙宫地区黑龙宫组和内蒙古达茂旗地区西别河组进行对比,自下而上具有相同的岩性和岩相变化规律。由上说明,二道沟组与小绥河组未发生倒转,属于正常层序,小绥河砂页岩层位高于二道沟灰岩。吉中地区西别河组层序自下而上为张家屯段-二道沟段-小绥河段。 展开更多
关键词 吉中地区 西别河组 地层层序 大陆边缘 佳-蒙地块
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Geomorphological Evolution Revealed by Aeolian Sedimentary Structure in Badain Jaran Desert on Alxa Plateau, Northwest China 被引量:7
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作者 BAI Yang WANG Nai'ang +1 位作者 LIAO Kongtai Patrick KLENK 《Chinese Geographical Science》 SCIE CSCD 2011年第3期267-278,共12页
The Badain Jaran Desert,located in the Alxa Plateau,Northwest China,features mega-dunes and a unique dune-lake alternation landscape.This paper presented the aeolian sediment structures of three representative dunes i... The Badain Jaran Desert,located in the Alxa Plateau,Northwest China,features mega-dunes and a unique dune-lake alternation landscape.This paper presented the aeolian sediment structures of three representative dunes in the Badain Jaran Desert using ground-penetrating radar (GPR).We processed and analyzed the GPR data and investigated the feasibility of using integrated GPR and sedimentological data to reconstruct dunes structure,sedimentary environment and geomorphological evolution.The results show that the internal structures of star dune and transverse dune represent various stages of mega-dune evolution: the main deposition processes of mega-dune are similar to those of transverse dunes but have a more complicated mechanism of sand transport and deposition because of the superimposition of dunes;the upper section of the mega-dune has a structure similar to that of star dune,with vertical aggradations on top.Diffraction hyperbolae in the GPR profile indicates that the presence of ancient dunes characterized by calcareous cementation layers is involved in the maintenance of mega-dunes,and water levels,shown by continuous,sub-horizontal GPR reflections,are supposed to be closely related to mega-dunes and the interdune lakes.Outcrop of wet sand and horizontal stratifications on the GPR image indicate moisture potentials with different levels inside mega-dunes.The multiplex geomorphology in the Badain Jaran Desert is the result of global climatic undulation,the unique geographical location,the geological structural features,etc. 展开更多
关键词 Badain Jaran Desert Ground-Penetrating Radar (GPR) mega-dunes sedimentary structure geomor- phological evolution
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Some conifers from Aptian in Yanbian area of Jilin, Northeast China 被引量:1
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作者 ZHAO Guowei SUN Yuewu ZHANG Ying 《Global Geology》 2013年第2期59-67,共9页
Some well-preserved conifer leafy shoots and female cones from the Lower Cretaceous Changcai For- mation near Fudong of Helong, eastern Jilin, Northeast China are studied. Based on gross morphological and cuticular st... Some well-preserved conifer leafy shoots and female cones from the Lower Cretaceous Changcai For- mation near Fudong of Helong, eastern Jilin, Northeast China are studied. Based on gross morphological and cuticular study, a new species, Elatides helongensis Sun et Zhao ( sp. nov. ) is described systematically. The new species is characterized by persistent, linear or slightly falcate leaves with obtusely acute apex, attached helically on the shoots. Female cones of the new species are terminal and oval, composed of persistent helically- arranged rhomboidal scales and erect seeds. One erect seed is growing on each scale. Leaf cuticles are hyposto- matic. Monocylic stomata are ellipse, composed of 2 sunken guard ceils and 4-8 subsidiary cells. Moreover, the cuticles of a young female cone of Pityostrobus yingchengensis Yang are described for the first time. 展开更多
关键词 Elatides Pityostrobus cuticle CRETACEOUS Changcai Formation
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An Empirical Study of Urban and Rural Integration Construction Development of Western Region in China --Taking Changji City of Xinjiang Autonomous Region as an Example
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作者 Jin Cailiang Jiang Xiuying 《International Journal of Technology Management》 2013年第12期22-24,共3页
The urban and rural integration is a new stage of city development, which is a process of urban and rural mutual supplementary integration, collaborative development and mutual prosperity. It takes the industry and ag... The urban and rural integration is a new stage of city development, which is a process of urban and rural mutual supplementary integration, collaborative development and mutual prosperity. It takes the industry and agriculture, city and countryside as a whole, with overall planning and coordination development, through system innovation and policy adjustment, in order to realize the integration development of urban and rural planning construction, industrial development, infrastructure, ecological environment and social career. This paper conducts the empirical analysis on the urban and rural integration construction development of Changji City of Changji Region in Xinjiang, studying the existing problems and restrictive factors of the process in promoting urban and rural integration construction in western region of China and trying to propose the corresponding countermeasures. 展开更多
关键词 Changji City of Xinjiang Autonomous Region urban and rural integration the existing problems the countermeasures
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