天然气地质学

准噶尔盆地玛湖凹陷早二叠世风城组沉积时期古湖盆卤水演化及碳酸盐矿物形成机理

展开
  • 1.中国石油大学(华东)地球科学与技术学院,山东 青岛 266580;
    2.中国石油勘探开发研究院杭州分院,浙江 杭州 310023;
    3.中国石油新疆油田分公司勘探开发研究院,新疆 克拉玛依 834000;
    4.中国石油新疆新港作业分公司,新疆 克拉玛依 834000
余宽宏(1983-),男,四川广元人,讲师,博士,主要从事沉积学及储层地质学研究. E-mail:yukuanhong@upc.edu.cn.

收稿日期: 2015-12-07

  修回日期: 2016-03-06

  网络出版日期: 2019-09-19

基金资助

山东省自然科学基金青年基金(编号:ZR2014DQ016);国家重点基础研究发展计划(“973”)(编号:2014CB239002);中国石油大学(华东)科研启动基金(编号:2013004);中央高校基本科研业务费专项资金(编号:16CX02030A)联合资助.

Brine evolution of ancient lake and mechanism of carbonate minerals during the sedimentation of Early Permian Fengcheng Formation in Mahu Depression,Junggar Basin,China

Expand
  • 1.School of Geosciences,China University of Petroleum,Qingdao 266580,China;
    2.Hangzhou Branch,Research Institute of Petroleum Exploration and Development,PetroChina,Hangzhou 310023,China;
    3.Research Institute of Exploration and Development,Xinjiang Oilfield Company,PetroChina,Karamay 834000,China;
    4.Xinjiang Xin’gang Operation Sub-Company,Xinjiang Oilfield Company,PetroChina,Karamay 834000,China

Received date: 2015-12-07

  Revised date: 2016-03-06

  Online published: 2019-09-19

摘要

准噶尔盆地西北缘玛湖凹陷风城组沉积时期古湖泊为典型的碳酸盐型湖泊,发育丰富的碳酸盐矿物。碳酸盐矿物是风城组主要的盐类矿物,可以按照金属阳离子划分为Mg、Ca碳酸盐(方解石、白云石)、Na碳酸盐(碳酸钠、碳酸氢钠)、过渡型碳酸盐(碳钠钙石、碳钠镁石、氯碳钠镁石)。3类碳酸盐矿物平面分布具有“牛眼”特征,表明蒸发浓缩是直接的成盐诱导因素。方解石、白云石主要分布在古湖盆的浅水平台区、湖盆的周缘浅水区。碳钠钙石、碳钠镁石、氯碳钠镁石主要分布在与碱矿互层的暗色沉凝灰岩层段。碳酸钠和碳酸氢钠主要分布在湖盆的凹陷中心。充足的HCO3-阴离子控制了玛湖凹陷古湖盆盐类矿物的沉淀,碳酸盐析盐序列表现为Mg2+、Ca2+首先与HCO3-结合,消耗殆尽后碱金属阳离子Na+与富余的HCO3-结合形成碱矿。早二叠世强烈的火山活动以及火山物质的矿物组成对碳酸盐矿物的形成起了决定性的作用。岛弧型火山活动脱气提供大量的CO2,增加了大气的CO2分压,进一步提高了沉积水体HCO3-浓度。HCO3-的含量是控制碳酸盐矿物沉淀的决定性因素。另外,火山喷发的CO2气体增加了降雨的酸度,并加速了对基岩的风化以及对火山碎屑物质的水解。准噶尔盆地西北缘石炭纪-早二叠世形成的火山岩富含Na长石分子及Ca长石分子,K长石分子含量低。风城组火山碎屑物质也以富含Na、Ca为主。基岩的风化以及凝灰质的水解提供了大量Na+、Ca2+、Mg2+、金属阳离子,与HCO3-结合形成了风城组大量的碳酸盐沉积。

本文引用格式

余宽宏, 操应长, 邱隆伟, 孙沛沛, 杨勇强, 曲长胜, 李玉文, 万敏, 宿云国 . 准噶尔盆地玛湖凹陷早二叠世风城组沉积时期古湖盆卤水演化及碳酸盐矿物形成机理[J]. 天然气地球科学, 2016 , 27(7) : 1248 -1263 . DOI: 10.11764/j.issn.1672-1926.2017.06.1248

Abstract

Saline minerals in Early Permian ancient Mahu lake,Junggar Basin were mainly carbonate minerals.Carbonate minerals in Fengcheng Formation covered 3 types according to positive metal ions,Mg-Ca carbonate minerals,calcite and dolomite,Na carbonate minerals,sodium carbonate,sodium bicarbonate,transitional carbonate minerals,shortite,eitelite,and northupite.The different kinds of carbonate minerals had regular horizontal distribution as bull’s-eye,which demonstrated that evaporation and concentration induced the deposition of carbonate minerals.Calcite and dolomite developed in shallow platform zone of Xiazijie area mainly and shallow lakemargin.Shortite,eitelite,and northupite developed in dark tuff layers which interbedded with alkali layers.Sodium carbonate and sodium bicarbonate developed in the center area of basin.Sufficient HCO3- negative ion controlled the evolution of brine of ancient Mahu lake.The Mg and Ca ions synthesized with HCO3- firstly and Na ions synthesized with residual HCO3- after calcite and dolomite precipitated.Intense volcanic activities and chemical compositions of Carboniferious-Early Permian igneous rocks and volcanic eruption materials played a decisive role for carbonate minerals precipitation.Island-arc volcanic eruptions delivered massive CO2,and increased PCO2 in atmosphere which improved HCO3- content in sedimentary water.In addition,CO2 in the atmosphere could promote bedrock weathering through rainfall and promote hydrolysis of tuff in sedimentary water with high HCO3-content.Igneous rocks around and basement of ancient Carboniferious-Early Permian Mahu lake,Northwest Junggar Basin were composed by albite molecules and Calcium feldspar molecules mainly,with low potassium feldspar molecules content.Volcanic clastic materials also had high Na and Ca content.Weathering of around Carboniferious-Early Permian igneous rocks and tuff hydrolysis offered plenty of Na,Ca,Mg ions,which synthesis with HCO3- and form various carbonate minerals.

参考文献

[1]James N P,Jones B.Origin of Carbonate Sedimentary Rocks[M].Hoboken:Wiley,2015:1-66.
[2]Jin Qiang,Zhu Guangyou,Wang Juan.Deposition and distribution of high-potential source rocks in saline lacustrine environments[J].Journal of China University of Petroleum,2008,32(4):19-23.[金强,朱光有,王娟.咸化湖盆优质烃源岩的形成与分布[J].中国石油大学学报:自然科学版,2008,32(4):19-23.]
[3]Yu Zhitong,Liu Xinqi,Wang Yong,et al.Evolution of Jilantai Salt Lake,Inner Mongolia in the last 13.8 ka[J].Journal of Lake Sciences,2012,24(4):629-636.[于志同,刘兴起,王永,等.13.8ka以来内蒙古吉兰泰盐湖的演化过程[J].湖泊科学,2012,24(4):629-636.]
[4]Feng Youliang,Zhang Yijie,Wang Ruiju,et al.Dolomites genesis and hydrocarbon enrichment of the Fengcheng Formation in the northwestern margin of Junggar Basin[J].Petroleum Exploration and Development,2011,38(6):685-692.[冯有良,张义杰,王瑞菊,等.准噶尔盆地西北缘风城组白云岩成因及油气富集因素[J].石油勘探与开发,2011,38(6):685-692.]
[5]Chen Lei,Ding Jing,Pan Weiqing,et al.Characteristics of high-quality reservoir and its controlling factorsof dolomitic rock in Fengcheng Formation of west slope in Junggar Basin
[J].China Petroleum Exploration,2012,17(3):8-11.[陈磊,丁靖,潘伟卿,等.准噶尔盆地玛湖凹陷西斜坡二叠系风城组云质岩优质储层特征及控制因素[J].中国石油勘探,2012,17(3):8-11.]
[6]Kuang Lichun,Tang Yong,Lei Dewen,et al.Formation conditions and exploration potential of tight oil in the Permian saline lacustrine dolomitic rock,Junggar Basin,NW China[J].Petroleum Exploration and Development,2012,39(6):657-667.[匡立春,唐勇,雷德文,等.准噶尔盆地二叠系咸化湖相云质岩致密油形成条件与勘探潜力[J].石油勘探与开发,2012,39(6):657-667.]
[7]Lu Xinchuan,Zhang Shuncun,Shi Ji’an.Dolomite genesis and geochemical characteristics of permian Fengcheng Formation in Wuerhe-Fengcheng area,northwestern Junggar Basin[J].Journal of Lanzhou University:Natural Sciences,2012,48(6):8-14.[鲁新川,张顺存,史基安.准噶尔盆地西北缘乌尔禾_风城地区二叠系风城组白云岩地球化学特征及成因分析[J].兰州大学学报:自然科学版,2012,48(6):8-14.]
[8]Xue Jingjing,Sun Jing,Zhu Xiaomin,et al.Characteristics and formation mechanism for dolomite reservoir of permian Fengcheng Formation in Junggar Basin[J].Geoscience,2012,26(4):755-761.[薛晶晶,孙靖,朱筱敏,等.准噶尔盆地二叠系风城组白云岩储层特征及成因机理分析[J].现代地质,2012,26(4):755-761.]
[9]Ying Jianguo,Ding Chao,Gu Qing,et al.Reservoir characteristics and controlling factors of dolomitic rocks of Fengcheng Formation in Wufeng area,northwestern margin of Juggar Basin[J].Lithologic Reservoirs,2012,24(5):83-88,106.[殷建国,丁超,辜清,等.准噶尔盆地西北缘乌风地区风城组白云质岩类储层特征及控制因素分析[J].岩性油气藏,2012,24(5):83-88,106.]
[10]Zhang Jie,Shou Jianfeng,Wen Yingchu,et al.Mechanism of dedolomitization and its rebuilding to reservoir[J].Journal of Palaeogeography,2012,14(1):69-84.[张杰,寿建峰,文应初,等.去白云石化作用机理及其对储集层的改造[J].古地理学报,2012,14(1):69-84.]
[11]Pan Xiaotian.Forming Mechanism of Fengcheng Formation of Lacustrine Hydrothermal Dolomite in the Junggar Basin in Northwestern Margin[D].Chengdu:Chengdu University of Technology(CDUT),2013:1-62.[潘晓添.准噶尔盆地西北缘风城组湖相热液白云岩形成机理[D].成都:成都理工大学,2013:1-62.]
[12]Pan Xiaotian,Zheng Rongcai,Wen Huaguo,et al.Tight oil reservoir of Permian Fengcheng Formation in Urho area,Junggar Basin,China[J].Journal of Chengdu University of Technology:Science & Technology Edition,2013,40(3):315-325.[潘晓添,郑荣才,文华国,等.准噶尔盆地乌尔禾地区风城组云质致密油储层特征[J].成都理工大学学报:自然科学版,2013,40(3):315-325.]
[13]Yin Lu,Qu Jianhua,Qi Liqi,et al.Lacustrine dolomitic pattern of permian in Fengcheng area in northwestern margin of Junggar Basin[J].Xinjiang Petroleum Geology,2013,34(5):542-544.[尹路,瞿建华,祁利祺,等.准噶尔盆地风城地区二叠系白云岩化模式[J].新疆石油地质,2013,34(5):542-544.]
[14]Zhu Shifa,Zhu Xiaomin,Tao Wenfang,et al.Origin of dolomitic reservoir rock in the Permian Fengcheng Formation in Wuxia area of the Junggar Basin[J].Geological Journal of China Universities,2013,19(1):38-45.[朱世发,朱筱敏,陶文芳,等.准噶尔盆地乌夏地区二叠系风城组云质岩类成因研究[J].高校地质学报,2013,19(1):38-45.]
[15]Gong Boshi,Wen Huaguo,Li Conglin,et al.Sedimentary environment of Fengcheng Formation in Urho area,Junggar Basin[J].Lithologic Reservoirs,2014,26(2):59-66.[宫博识,文华国,李丛林,等.准噶尔盆地乌尔禾地区风城组沉积环境分析[J].岩性油气藏,2014,26(2):59-66.]
[16]Liu Yinghui,Zhu Xiaomin,Zhu Mao,et al.Characteristics of tight oil reservoirs of the Permian Fengcheng Formation in Wuxia area,Junggar Basin[J].Lithologic Reservoirs,2014,26(4):66-72.[刘英辉,朱筱敏,朱茂,等.准噶尔盆地乌—夏地区二叠系风城组致密油储层特征[J].岩性油气藏,2014,26(4):66-72.]
[17]Wang Junhuai,Liu Yinghui,Wan Ce,et al.Characteristics and origin of dolomitic tuff in the Permian Fengcheng Formation in Wuxia area of Junggar Basin[J].Journal of Palaeogeography,2014,16(2):157-168.[王俊怀,刘英辉,万策,等.准噶尔盆地乌—夏地区二叠系风城组云质岩特征及成因[J].古地理学报,2014,16(2):157-168.]
[18]Zhu Shifa,Zhu Xiaomin,Liu Yinghui,et al.Petrological and geochemical features of dolomitic rocks in the Lower Permian Fengcheng Formation in Wuerhe-Xiazijie area,Junggar Basin[J].Geological Review,2014,60(5):1113-1122.[朱世发,朱筱敏,刘英辉,等.准噶尔盆地西北缘北东段下二叠统风城组白云质岩岩石学和岩石地球化学特征[J].地质论评,2014,60(5):1113-1122.]
[19]Fu Rao,Zheng Rongcai,Chang Hailiang,et al.Lacustrine “white smoke type” exhalative rock:A new type of tight oil reservoir:A case study from Lower Permian Fengcheng Formation in Urho area,western margin of Junggar Basin[J].Lithologic Reservoirs,2015,27(3):32-42.[傅饶,郑荣才,常海亮,等.湖相“白烟型”喷流岩——新型的致密油储层类型——以准噶尔盆地西缘乌尔禾地区风城组为例[J].岩性油气藏,2015,27(3):32-42.]
[20]Jia Bin,Wen Huaguo,Li Yingbo,et al.Fluid inclusions in the salt minerals from the Permian Fengcheng Formation in the Urho region,Junggar Basin,Xinjiang[J].Sedimentary Geology and Tethyan Geology,2015,35(1):33-42.[贾斌,文华国,李颖博,等.准噶尔盆地乌尔禾地区二叠系风城组盐类矿物流体包裹体特征[J].沉积与特提斯地质,2015,35(1):33-42.]
[21]Cao Jian,Lei Dewen,Li Yuwen,et al.Ancient high-quality alkaline lacustrine source rocks discovered in the Lower Permian Fengcheng Formation,Junggar Basin[J].Acta Petrolei Sinica,2015,36(7):781-790.[曹剑,雷德文,李玉文,等.古老碱湖优质烃源岩:准噶尔盆地下二叠统风城组[J].石油学报,2015,36(7):781-790.]
[22]Abulimiti,Cao Jian,Chen Jing,et al.Origin and Occurrence of highly matured oil and gas in Mahu Sag,Junggar Basin[J].Xinjiang Petroleum Geology,2015,36(4):379-384.[阿布力米提,曹剑,陈静,等.准噶尔盆地玛湖凹陷高成熟油气成因与分布[J].新疆石油地质,2015,36(4):379-384.]
[23]Wu Kongyou,Zha Min,Wang Xulong,et al.Further researches on the tectonic evolution and dynamic setting of the Junggar Basin[J].Acta Geoscientica Sinica,2005,26(3):217-222.[吴孔友,查明,王绪龙,等.准噶尔盆地构造演化与动力学背景再认识[J].地球学报,2005,26(3):217-222.]
[24]Ma Zongjin,Qu Guosheng,Li Tao,et al.Tectonic coupling and segmentation of marginal structural belt in Junggar Basin[J].Xinjiang Petroleum Geology,2008,29(3):271-277.[马宗晋,曲国胜,李涛,等.准噶尔盆地盆山构造耦合与分段性[J].新疆石油地质,2008,29(3):271-277.]
[25]Zou Niuniu,Zhang Daquan,Wu Tao,et al.Reservoir characteristics and controlling factors in the dolomitic clastic rocks of Fengcheng Formation in northwestern Juggar Basin[J].Natural Gas Geoscience,2015,26(5):861-870.[邹妞妞,张大权,吴涛,等.准噶尔西北缘风城组云质碎屑岩类储层特征及控制因素[J].天然气地球科学,2015,26(5):861-870.]
[26]Jiang Yiqin,Wen Huaguo,Qi Liqi,et al.Salt minerals and their genesis of the permian fengcheng formation in urho area,Junggar Basin[J].Journal of Mineralogy and Petrology,2012,32(2):105-114.[蒋宜勤,文华国,祁利祺,等.准噶尔盆地乌尔禾地区二叠系风城组盐类矿物和成因分析[J].矿物岩石,2012,32(2):105-114.]
[27]Eugster H P.Geochemistry of evaporitic lacustrine deposits[J].Annual Review of Earth and Planetary Sciences,1980(8):35-63.
[28]Huang Chunju,Chen Kaiyuan,Yang Xianghua.Characteristics of sequence stratigraphy in the saline lake basin[J].Oil & Gas Geology,2002,23(2):134-138.[黄春菊,陈开远,杨香华.盐湖盆地层序地层特征[J].石油与天然气地质,2002,23(2):134-138.]
[29]Wang Guoli,Yang Yuqing,Zhang Yongsheng,et al.Sedimentary microfacies and evolution of the Qianjiang Formation of Paleogene at Wangchang area in Qianjiang Sag,Jianghan Basin[J].
Journal of Palaeogeography,2004,6(2):140-150.[王国力,杨玉卿,张永生,等.江汉盆地潜江凹陷王场地区古近系潜江组沉积微相及其演变[J].古地理学报,2004,6(2):140-150.]
[30]Yuan Jianqi,Huo Chungyu,Cai Keqin.
The high mountain-deep basin saline environment:A new genetic model of salt deposits[J].Geological Review,2012,29(2):159-165.[袁见齐,霍承禹,蔡克勤.高山深盆的成盐环境——一种新的成盐模式的剖析[J].地质论评,2012,29(2):159-165.]
[31]Shi Hui,Liu Zhen,Lian Liangda,et al.Enrichment ragularity of lithologic reservoirs in plateau saline lacustrine basin:Taking the southwestern Qaidam Basin for example[J].
Natural Gas Geoscience,2013,24(4):701-711.[施辉,刘震,连良达,等.高原咸化湖盆岩性油气藏富集规律——以柴达木盆地西南区为例[J].天然气地球科学,2013,24(4):701-711.]
[32]Wang Sumin.Physics and chemistry of saline lakes[J].Journal of Lake Sciences,1993,5(3):278-286.[王苏民.世界咸水湖的物理与化学特性[J].湖泊科学,1993,5(3):278-286.]
[33]Türkmen ,zkul M.Sedimentology and evaporite genesis of neogene continental sabkha playa complex,Karakecili Basin,Central Anatolia,Turkey[J].Carbonates & Evaporites,1999,14(1):21-31.
[34]Zhu Huaicheng,Ouyang Shu,Zhan Jiazhen,et al.Comparison of Permian palynological assemblages from the Junggar and Tarim Basins and their phytoprovincial significance[J].Review of Palaeobotany & Palynology,2005,136(3):181-207.
[35]Li Wei.Formation of a saline environment and evolution of a sedimentary system in the Late Triassic reservoir of the Sichuan Basin[J].Natural Gas Industry,2011,31(9):31-38.[李伟.四川盆地晚三叠世咸化环境的形成与沉积体系的演化特征[J].天然气工业,2011,31(9):31-38.]
[36]Neev D,Emery K D.The Dead Sea Depositional processes and environments of evaporates[J].Israel Geol.Surv Bull.,1967,41:147.
[37]Zhao Jingfeng,Qin Dahe,Lei Jiaqiang,et al.Inter-annual Variability of salt budget of the Yanqi Basin and Lake Bosten,Xinjiang[J].Arid Land Geography,2005,28(3):275-281.[赵景峰,秦大河,雷加强,等.新疆焉耆盆地和博斯腾湖盐量收支平衡的年变化[J].干旱区地理,2005,28(3):275-281.]
[38]Chen Shiyue,Wang Ling,Li Cong,et al.The saline genesis of lacustrine basin in the lower section of the first member of Shahejie Formation in Qikou Sag[J].Acta Petrolei Sinca,2012,33(1):40-47.[陈世悦,王玲,李聪,等.歧口凹陷古近系沙河街组一段下亚段湖盆咸化成因[J].石油学报,2012,33(1):40-47.]
[39]Xue Guogang,Gao Jianzhen.Volcanism and halite genesis in Shahejie Formation of paleaogene in Dongpu Depression[J].Journal of Oil and Gas Technology,2011,33(1):53-56,75.[薛国刚,高渐珍.东濮凹陷古近系沙河街组火山作用与盐岩成因[J].石油天然气学报,2011,33(1):53-56,75.]
[40]Yuan Jing,Zhao Chenglin,Zhang Shanwen.Genetic model of the deep water salt lake of the Paleogene Sha-4 member in Dongying Sag[J].Acta Sedimentologica Sinica,2000,18(1):114-118.[袁静,赵澄林,张善文.东营凹陷沙四段盐湖的深水成因模式[J].沉积学报,2000,18(1):114-118.]
[41]Jin Qiang.Geochemistry characteristics of trace elements in evaporates of the Tertiary[J].Journal of the University of Petroleum,China:Edition of Natural Scinece,2003,27(2):1-5.[金强.柴达木盆地西部第三系蒸发岩微量元素组成及其地球化学特征[J].石油大学学报:自然科学版,2003,27(2):1-5.]
[42]Jin Qiang,Zhu Guangyou.Progress in research of deposition of oil source rocks in saline lakes and their hydrocarbon generation[J].Geological Journal of China Universities,2006,12(4):483-492.[金强,朱光有.中国中新生代咸化湖盆烃源岩沉积的问题及相关进展[J].高校地质学报,2006,12(4):483-492.]
[43]Zheng Xiyu,Lv Yaping.Salt lakes and carbonate origin in Hailar Basin[J].Journal of Salt Lake Science,1995,3(3):1-10.[郑喜玉,吕亚平.海拉尔盆地盐湖及碳酸盐成因[J].盐湖研究,1995,3(3):1-10.]
[44]Zheng Xiyu,Lv Yaping.Formation and evolution environment of dabusu alkaline lake[J].Journal of Salt Lake Science,1995,3(4):10-17.[郑喜玉,吕亚平.大布苏碱湖的形成演化环境[J].盐湖研究,1995,3(4):10-17.]
[45]Jia Guodong,Cai Keqin.Biogeochemical process during soda mineralization in the hetong qahan nur soda lake,Inner Mongolia[J].Geological Review,2012,43(4):388-393.[贾国东,蔡克勤.内蒙古合同察汗淖碱湖成碱过程中的生物地球化学作用[J].地质论评,2012,43(4):388-393.]
[46]Yang Qingtang.Modern salt lakes in yikezhao league,inner mongolia:Geological characteristics and trona-forming conditions[J].Geology of Chemical Minerals,1996,18(1):31-38.[杨清堂.内蒙古伊盟地区现代碱湖地质特征和形成条件分析[J].化工矿产地质,1996,18(1):31-38.]
[47]Sun Dapeng.The soda lakes on inner monggolia plateau,China[J].Oceanologia Et Limnologia Sinica,1990,21(1):44-54.[孙大鹏.内蒙高原的天然碱湖[J].海洋与湖沼,1990,21(1):44-54.]
[48]Zheng Dazhong,Zheng Ruofeng.Preliminary investigation of natural alkaline deposits and the formation mechanism of their salt lakes[J].Journal of Salt Lake Research,2002,10(2):1-9.[郑大中,郑若锋.天然碱矿床及其盐湖形成机理初探[J].盐湖研究,2002,10(2):1-9.]
[49]Huang Xinzhen,Yan Cunfeng,Wang Suiji,et al.The feature and deposit model of lacustrine carbonate rocks formed in the course of soda lake evolution[J].Acta Sedimentologica Sinica,1999,17(supplement 1):728-733.[黄杏珍,闫存凤,王随继,等.苏打湖型的湖相碳酸盐岩特征及沉积模式[J].沉积学报,1999,17(增刊1):728-733.]
[50]Coffey M T,Mankin W G.Volcanoes:Composition of Emissions[M].Encyclopedia of Atmospheric Sciences(volume 1).2nd Edition.2015:446-449.
[51]Wiliams S N,Schaefer S J,Lopez M L,et al.Global carbon dioxide emission to the atmosphere by volcanoes[J].Geochimica et Cosmochimica Acta,1992,56:1765-1770.
[52]Hernández P A,Melián G,Giammanco S,et al.Contribution of CO2 and H2S emitted to the atmosphere by plume and diffuse degassing from volcanoes:The Etna volcano case study[J].Surveys in Geophysics,2015,36(3):327-349.
[53]Xu Qinqin,Ji Jianqing,Zhao Lei,et al.Tectonic evolution and continental crust growth of northern Xinjiang in northwestern China:Remnant ocean model[J].Earth-Science Reviews,2013,126:178-205.
[54]Choulet F,Michel F,Dominique C,et al.Toward a unified model of Altaids geodynamics:Insight from the Palaeozoic polycyclic evolution of west Junggar(NW China)[J].Science China Earth Sciences,2015,59(1):25-57.
[55]Li Di,He D F,Santosh M,et al.Tectonic framework of the northern Junggar Basin part Ⅰ:The eastern Luliang Uplift and its link with the east Junggar terrane[J].Gondwana Research,2015,27(3):1089-1109.
[56]Li D,He D F,Santosh M,et al.Tectonic framework of the northern Junggar Basin Part Ⅱ:The island arc basin system of the western Luliang Uplift and its link with the West Junggar terrane[J].Gondwana Research,2015,27(3):1110-1130.
[57]Yin J Y,Long X P,Yuan C,et al.A Late Carboniferous-Early Permian slab window in the west Junggar of NW China:Geochronological and geochemical evidence from mafic to intermediate dikes[J].Lithos,2013,(175/176):146-162.
[58]Pirajno F,Seltmann R,Yang Y Q.A review of mineral systems and associated tectonic settings of northern Xinjiang,NW China[J].Geoscience Frontiers,2011,2(2):157-185.
[59]Zhan Y,Hou G T,Hari K R,et al.Geochemical and isotopic constraints on the evolution of Late Paleozoic dyke swarms in West Junggar,Xinjiang,China[J].Journal of Asian Earth Sciences,2014,113:126-136.
[60]Xiao W J,Han C M,Yuan C,et al.Middle Cambrian to Permian subduction-related accretionary orogenesis of Northern Xinjiang,NW China:Implications for the tectonic evolution of central Asia[J].Journal of Asian Earth Sciences,2008,32(2-4):102-117.
[61]Bian W H,Hornung J,Liu Z H,et al.Sedimentary and palaeoenvironmental evolution of the Junggar Basin,Xinjiang,northwest China[J].Palaeobiodiversity & Palaeoenvironments,2010,90(3):175-186.
[62]Lu X C,Shi J A,Zhang Shuncun,et al.The origin and formation model of Permian dolostones on the northwestern margin of Junggar Basin,China[J].Journal of Asian Earth Sciences,2015,105:456-467.
[63]Zhang J E,Xiao W J,Han C M,et al.A Devonian to Carboniferous intra-oceanic subduction system in western Junggar,NW China[J].Lithos,2011,125(1/2):592-606.
[64]Gao R,Xiao L,Pirajno F,et al.Carboniferous-Permian extensive magmatism in the West Junggar,Xinjiang,northwestern China:Its geochemistry,geochronology,and petrogenesis[J].Lithos,2014,204:125-143.
[65]Yang G X,Li Y J,Gu P Y,et al.Geochronological and geochemical study of the Darbut Ophiolitic Complex in the West Junggar(NW China):Implications for petrogenesis and tectonic evolution[J].Gondwana Research,2012,21(4):1037-1049.
[66]Zhu Shifa,Zhu Xiaomin,Liu Jishan,et al.Genesis and hydrocarbon significance of vesicular ignimbrite:A case study from Fengcheng Formation,Wu-Xia area,Junggar Basin,NW China[J].Petroleum Exploration and Development,2012,39(2):162-171.[朱世发,朱筱敏,刘继山,等.富孔熔结凝灰岩成因及油气意义——以准噶尔盆地乌—夏地区风城组为例[J].石油勘探与开发,2012,39(2):162-171.]
[67]Zheng J P,Sun M,Zhao G C,et al.Elemental and Sr-Nd-Pb isotopic geochemistry of Late Paleozoic volcanic rocks beneath the Junggar basin,NW China:Implications for the formation and evolution of the basin basement[J].Journal of Asian Earth Sciences,2007,29(5/6):778-794.
[68]Mason R.A.The Ordering Behaviour of Reedmergnerite,NaBSi3O8[J].Contributions to Mineralogy and Petrology,1980(72):329-333.
[69]Chen J,Wang H N.Geochemistry[M].Beijing:Science Press,2004:396-400.[陈俊,王鹤年.地球化学[M].北京:科学出版社,2004:396-400.]
[70]Xu X S,Qiu J S.Igneous Petrology[M].Beijing:Science Press,2010:270.[徐夕生,邱检生.火成岩岩石学[M].北京:科学出版社,2010:270.]

文章导航

/