甘肃阿尔金南缘白石头沟石墨矿地质特征、成矿条件及找矿标志
|
摘要
甘肃白石头沟石墨矿位于阿尔金南缘敦煌地块,赋存于前寒武纪敦煌岩群大理岩和石英片岩之中,目前圈定矿体33条,主要矿体2条。作为研究白石头沟石墨矿理想地层的敦煌岩群,是一套以变质碎屑沉积岩和变质基性岩为主的变质岩浆杂岩。本文从矿床角度出发,立足于区域地质勘查资料,结合前人研究成果,在对白石头沟石墨矿成矿地质背景、矿床及矿体特征、组合样化学分析、矿石矿物赋存状态及特征研究的基础上,对矿床的成因进行初步探讨并归纳区域找矿标志。研究表明,白石头沟石墨矿可分为大理岩型和石英片岩型两种类型,是古元古代经历区域动力热液变质作用而形成的沉积变质型矿床,成矿物质主要来源于变质碎屑沉积岩类的原岩(海相陆源碎屑岩和碳酸盐岩)本身,成矿环境为古老活动大陆边缘。找矿标志具有特定层位、岩性、矿化及物探特征。
The Baishitougou graphite deposit is located at the Dunhuang block in the southern margin of the Altun,and occurs in marble and quartz schist of the Precambrian Dunhuang group. So far,33 ore bodies,including 2 main ore bodies,have been delineated. As an ideal stratum for study of the Baishitougou graphite deposit,the Dunhuang group is a set of metamorphic magmatic complexes dominated by metamorphic clastic sedimentary rocks and metamorphic basic rocks. This article presents a preliminary discussion on the genesis of the deposit and summarizes the ore-prospecting signs from the perspective of the deposit and regional geological survey data,in combination with previous work. It is also based on the research of mineralization geological background of the deposit,features of the deposit and ore-bodies,analysis of composite samples,ore mineral occurrence state and characteristics. The research shows that the Baishitougou graphite deposit can be divided into two types: marble type and quartz schist type. It is a sedimentary metamorphic deposit formed by regional dynamic hydrodynamic metamorphism in the Palaeoproterozoic. The ore-forming material was mainly derived from the protolith of the metamorphic clastic sedimentary rocks( marine terrigenous clastic rock and carbonate). Its metallogenic environment was an ancient active continental margin. The ore-prospecting signs in this area have special horizons,lithology,mineralization,and geophysical features.
The Baishitougou graphite deposit is located at the Dunhuang block in the southern margin of the Altun,and occurs in marble and quartz schist of the Precambrian Dunhuang group. So far,33 ore bodies,including 2 main ore bodies,have been delineated. As an ideal stratum for study of the Baishitougou graphite deposit,the Dunhuang group is a set of metamorphic magmatic complexes dominated by metamorphic clastic sedimentary rocks and metamorphic basic rocks. This article presents a preliminary discussion on the genesis of the deposit and summarizes the ore-prospecting signs from the perspective of the deposit and regional geological survey data,in combination with previous work. It is also based on the research of mineralization geological background of the deposit,features of the deposit and ore-bodies,analysis of composite samples,ore mineral occurrence state and characteristics. The research shows that the Baishitougou graphite deposit can be divided into two types: marble type and quartz schist type. It is a sedimentary metamorphic deposit formed by regional dynamic hydrodynamic metamorphism in the Palaeoproterozoic. The ore-forming material was mainly derived from the protolith of the metamorphic clastic sedimentary rocks( marine terrigenous clastic rock and carbonate). Its metallogenic environment was an ancient active continental margin. The ore-prospecting signs in this area have special horizons,lithology,mineralization,and geophysical features.
引文
Bai Jianke,Chen Junlu,Peng Suxia.2017.Characteristics and metallogeny regulation of graphite resources in Xinjiang[J].Acta Geologica Sinica,91(12):2828-2840(in Chinese with English abstract).
Bao Weihang.2017.The Precambrian and Late Paleozoic continental crust evolution in the south margin of the Dunhuang block[D].Guangzhou:University of Chinese Academy of Sciences(Guangzhou Institute of Geochemistry):1-89(in Chinese with English abstract).
Huang An.2017.The research on the origin of the Chahanmuhulu graphite deposit in Inner Mongolia autonomous region[D].Beijing:China University of Geosciences(Beijing):1-51(in Chinese).
Jiang Gaozhen,Li Yike,Wang Anjian,Yang Xuan,Yang Biao,Ma Li.2017.Genetic features of Dawudian graphite deposit in Urad Middle Banner,Inner Mongolia[J].Earth Science Frontiers,24(5):306-316(in Chinese with English abstract).
Li Chao,Wang Denghong,Zhao Hong,Pei Haoxiang,Li Xinwei,Zhou Limin,Du Andao,Qu Wenjun.2015.Minerogenetic regularity of graphite deposits in China[J].Mineral Deposits,34(6):1223-1236.(in Chinese with English abstract).
Li Siyuan.2017.Resource distribution and genesis of natural crystalline graphite in Heilongjiang[D].Beijing:China University of Geosciences(Beijing):1-62(in Chinese with English abstract).
Liang Shuai.2015.Genisis studies of typical crystalline graphite deposits in North China[D].Fuxin:Liaoning Technical University:1-124(in Chinese).
Lu Songnian,Li Huaikun,Zhang Chuanlin,Niu Guanghua.2008.Geological and geochronological evidence for the Precambrian evolution of the Tarim Craton and surrounding continental fragments[J].Precambrian Research,160(1-2):94-107.
Lu Yaozu,Xu Jiaqiu.2018.Graphite mineralization characteristics and prospecting potential analysis of Jinghongshan-Eboliang area in Altunshan area[J].Contributions to Geology and Mineral Resources Research,33(01):23-30(in Chinese).
Mei Hualin,Yu Haifeng,Lu Songnian,Li Huimin,Li Shuan,Lin Yuanxian,Zuo Yicheng.1998.Archean tonalite in the Dunhuang,Gansu Province:Age from the U-Pb single zircon and Nd isotope[J].Progress in Precamrian Research,(02):41-45(in Chinese).
Meng Fancong,Zhang Jianxin,Xiang Zhenqun,Yu Shengyao,Li Jinping.2011.Evolution and formation of the Dunhuang group in NE Tarim basin,NW China:Evidence from detrital-zircon geochronology and Hf isotope[J].Acta Petrologica Sinica,27(1):59-76(in Chinese with English abstract).
Shi Mengyan,Hou Quanlin,Wu Chunming,Wang Hao,Chen Hongxu.2017.An analysis of the characteristics of the rock-structure association of the Dunhuang orogenic belt and their implications for tectonic setting[J].Geological Bulletin of China,36(2-3):238-250(in Chinese with English abstract).
Tang Hejun,Zhang Baolin,Ye Rong,Zhang Guoliang,Zhang Wenbin.2015.Geological characteristics and genesis of the Miaoping graphite deposit in Mian county of Shaanxi Province[J].Geology and Exploration,51(3):534-544(in Chinese with English abstract).
Wang Jingyong.2008.Identification of granitic orthogneiss of Dunhuang rock group in Xiadong area of Gansu Province and its significance[J].Gansu Geology,(3):22-26(in Chinese).
Wang Nan,Wu Cailai,Ma Changqian,Lei Min,Guo Wenfeng,Zhang Xi,Chen Hongjie.2016.Geochemistry,zircon U-Pb geochronology and Hf isotopic characteristics for Granites in southern Dunhuang block[J].Acta Petrologica Sinica,32(11):3753-3780(in Chinese with English abstract).
Wang Yong,Wang Bin,Chen Bailin,Wu Yu,Meng Lingtong,He Jiangtao,Chen Andong.2017.New evidence of 2.0-1.8 Ga granitic genesis Tarim plate belonging to Colombia supercontinent[J].Geology in China,44(2):407-408(in Chinese with English abstract).
Wang Zhongmei,Han Chunming,Su Benxun,Patrick Asamoah Sakyi,Sanjeewa Malaviarachchi,Ao Songjian,Wang Luojuan.2013.The metasedimentary rocks from the eastern margin of the Tarim Craton:Petrology,geochemistry,zircon U-Pb dating,Hf isotopes and tectonic implications[J].Lithos,179:120-136.
Wang Zhongmei,Han Chunming,Xiao Wenjiao,Wan Bo,Patrick Asamoah Sakyi,Ao Songjian,Zhang Ji'en,Song Dongfang.2014.Petrology and geochronology of Paleoproterozoic garnet-bearing amphibolites from the Dunhuang block,eastern Tarim Craton[J].Precambrian Research,255:163-180.
Xin Houtian,Liu Yongshun,Luo Zhaohua,Song Shunchang,Wang Shuqing.2013.The growth of Archean continental crust in Aqtashtagh area of southeast Tarim,China:Constraints from petrochemistry and chronology about Milan group and TTG-gneiss[J].Earth Science Frontiers,20(1):240-259(in Chinese with English abstract).
Xu Zhiqin,Yang Jingsui,Zhang Jianxin,Jiang Mei,Li Haibing,Cui Junwen.1999.A comparison between the tectonic units on the two sides of the Altun sinistral strike-slip fault and the mechanism of lithospheric shearing[J].Acta Geologica Sinica,(3):193-205(in Chinese).
Yan Lingya,Gao Shuxue,Chen Zhengguo,Jiao Lixiang,Sun Li,Liu Yanfei,Zhou Wen.2018.Metallogenic characteristics and metallogenic zoning of graphite deposits in China[J].Geology in China,45(3):421-440(in Chinese with English abstract).
Zhang Jianxin,Gong Jianghua,Yu Shengyao.2012.1.85Ga HP granulitefacies metamorphism in the Dunhuang block of the Tarim Craton,NW China:Evidence from U-Pb zircon dating of mafic granulites[J].Journal of the Geological Society,London,169(5):511-514.
Zhang Jianxin,Li Huaikun,Meng Fancong,Xiang Zhenqun,Yu Shengyao,Li Jinping.2011.Polyphase tectonothermal events recorded in“metamorphic basement”from the Altyn Tagh,the southeastern margin of the Tarim basin,western China:Constraint from U-Pb zircon geochronology[J].Acta Petrologica Sinica,27(1):23-46(in Chinese with English abstract).
Zhang Jianxin,Yu Shengyao,Gong Jianghua,Li Huaikun,Hou Kejun.2013.The latest Neoarchean-Paleoproterozoic evolution of the Dunhuang block,eastern Tarim craton,northwestern China:Evidence from zircon U-Pb dating and Hf isotopic analyses[J].Precambrian Research,226(1):21-42.
Zhang Tengfei.2015.The geochemical characteristics and deposit genesis analysis of Xiaochagou graphite deposit in Zhenping County of Henan Province[D].Beijing:China University of Geosciences(Beijing):1-70(in Chinese).
Zhao Yan,Diwu Chunrong,Sun Yong,Zhu Tao,Wang Hongliang.2013.Zircon geochronology and Lu-Hf isotope composition for Precambrian rocks of the Dunhuang complex in Shuixiakou area,Gansu Province[J].Acta Petrologica Sinica,29(05):1698-1712(in Chinese with English abstract).
Zhao Yan,Sun Yong,Yan Jianghao,Diwu Chunrong.2015.The ArcheanPaleoproterozoic crustal evolution in the Dunhuang region,NW China:Constraints from zircon U-Pb geochronology and in situ Hf isotopes[J].Precambrian Research,271:83-97.
Zhao Yan.2017.Composition and evolution of the Dunhuang orogenic belt[D].Xi'an:Northwest University:1-373(in Chinese).
Zong Keqing,Liu Yongsheng,Zhang Zeming,He Zhenyu,Hu Zhaochu,Guo Jingliang,Chen Kang.2013.The generation and evolution of Archean continental crust in the Dunhuang block,northeastern Tarim Craton,northwestern China[J].Precambrian Research,235:251-263.
Zhao Zhenming,Ji Wenhua,Li Wenming.2018.Metamorphic Genesis of Magnetite Quartzite with Iron Mineralization in the Dunhuang group of southern Beishan region[J].Geology and Exploration,54(4):689-701(in Chinese with English abstract).
白建科,陈隽璐,彭素霞.2017.新疆石墨资源特征及成矿规律[J].地质学报,91(12):2828-2840.
包伟航.2017.敦煌地块南缘前寒武纪及晚古生代大陆地壳演化[D].广州:中国科学院大学(中国科学院广州地球化学研究所):1-89.
甘肃省地质矿产局.1989甘肃省区域地质志[M].北京:地质出版社:1-692.
黄安.2017.内蒙古自治区查汗木胡鲁石墨矿矿床成因研究[D].北京:中国地质大学(北京):1-51.
姜高珍,李以科,王安建,杨轩,杨彪,马莉.2017.内蒙古乌拉特中旗大乌淀石墨矿成因特征分析[J].地学前缘,24(5):306-316.
李超,王登红,赵鸿,裴浩翔,李欣尉,周利敏,杜安道,屈文俊.2015.中国石墨矿床成矿规律概要[J].矿床地质,34(6):1223-1236.
李思远.2017.黑龙江省天然晶质石墨资源分布及矿床成因研究[D].北京:中国地质大学(北京):1-62.
梁帅.2015.华北典型晶质石墨矿床成因研究[D].阜新:辽宁工程技术大学:1-124.
路耀祖,徐加求.2018.阿尔金南缘金鸿山-俄博梁地区石墨矿化特征及找矿前景分析[J].地质找矿论丛,33(1):23-30.
梅华林,于海峰,陆松年,李惠民,李铨,林源贤,左义成.1998.甘肃敦煌太古宙英云闪长岩:单颗粒锆石U-Pb年龄和Nd同位素[J].前寒武纪研究进展,(2):41-45.
孟繁聪,张建新,相振群,于胜尧,李金平.2011.塔里木盆地东北缘敦煌群的形成和演化:锆石U-Pb年代学和Lu-Hf同位素证据[J].岩石学报,27(1):59-76
石梦岩,侯泉林,吴春明,王浩,陈泓旭.2017.敦煌造山带岩石-构造组合特征及其构造环境[J].地质通报,36(2-3):238-250.
汤贺军,张宝林,叶荣,张国梁,张文斌.2015.陕西勉县庙坪石墨矿床地质特征与成因初步探讨[J].地质与勘探,51(3):534-544.
王静永.2008.甘肃北山南带峡东地区敦煌岩群中花岗质正片麻岩的确认及其意义[J].甘肃地质,(03):22-26.
王楠,吴才来,马昌前,雷敏,郭文峰,张昕,陈红杰.2016.敦煌地块南部古生代花岗岩地球化学、锆石U-Pb定年及Hf同位素特征研究[J].岩石学报,32(12):3753-3780.
王永,王斌,陈柏林,吴玉,孟令通,何江涛,陈安东.2017.塔里木板块归属Colombia超大陆的新证据:来自北阿尔金地区2.0~1.8 Ga花岗质片麻岩体[J].中国地质,44(02):407-408.
辛后田,刘永顺,罗照华,宋顺昌,王树庆.2013.塔里木盆地东南缘阿克塔什塔格地区新太古代陆壳增生:米兰岩群和TTG片麻岩的地球化学及年代学约束[J].地学前缘,20(1):240-259
许志琴,杨经绥,张建新,姜枚,李海兵,崔军文.1999.阿尔金断裂两侧构造单元的对比及岩石圈剪切机制[J].地质学报,(03):193-205.
颜玲亚,高树学,陈正国,焦丽香,孙莉,刘艳飞,周雯.2018.中国石墨矿成矿特征及成矿区带划分[J].中国地质,45(03):421-440.
郁东良,王永刚,申大利.2016.柴达木盆地西北缘晶质石墨矿特征及找矿远景[J].现代矿业,32(09):179-181.
张建新,李怀坤,孟繁聪,相振群,于胜尧,李金平.2011.塔里木盆地东南缘(阿尔金山)“变质基底”记录的多期构造热事件:锆石U-Pb年代学的制约[J].岩石学报,27(1):23-46.
张腾飞.2015.河南省镇平县小岔沟石墨矿矿床地球化学特征及成因分析[D].北京:中国地质大学(北京):1-70.
赵燕,第五春荣,孙勇,朱涛,王洪亮.2013.甘肃敦煌水峡口地区前寒武纪岩石的锆石U-Pb年龄、Hf同位素组成及其地质意义[J].岩石学报,29(05):1698-1712.
赵燕.2017.敦煌造山带的构成及演化[D].西安:西北大学:1-373.
赵振明,计文化,李文明.2018.北山南部敦煌岩群铁矿化磁铁石英岩的变质成因[J].地质与勘探,54(04):689-701.
Bao Weihang.2017.The Precambrian and Late Paleozoic continental crust evolution in the south margin of the Dunhuang block[D].Guangzhou:University of Chinese Academy of Sciences(Guangzhou Institute of Geochemistry):1-89(in Chinese with English abstract).
Huang An.2017.The research on the origin of the Chahanmuhulu graphite deposit in Inner Mongolia autonomous region[D].Beijing:China University of Geosciences(Beijing):1-51(in Chinese).
Jiang Gaozhen,Li Yike,Wang Anjian,Yang Xuan,Yang Biao,Ma Li.2017.Genetic features of Dawudian graphite deposit in Urad Middle Banner,Inner Mongolia[J].Earth Science Frontiers,24(5):306-316(in Chinese with English abstract).
Li Chao,Wang Denghong,Zhao Hong,Pei Haoxiang,Li Xinwei,Zhou Limin,Du Andao,Qu Wenjun.2015.Minerogenetic regularity of graphite deposits in China[J].Mineral Deposits,34(6):1223-1236.(in Chinese with English abstract).
Li Siyuan.2017.Resource distribution and genesis of natural crystalline graphite in Heilongjiang[D].Beijing:China University of Geosciences(Beijing):1-62(in Chinese with English abstract).
Liang Shuai.2015.Genisis studies of typical crystalline graphite deposits in North China[D].Fuxin:Liaoning Technical University:1-124(in Chinese).
Lu Songnian,Li Huaikun,Zhang Chuanlin,Niu Guanghua.2008.Geological and geochronological evidence for the Precambrian evolution of the Tarim Craton and surrounding continental fragments[J].Precambrian Research,160(1-2):94-107.
Lu Yaozu,Xu Jiaqiu.2018.Graphite mineralization characteristics and prospecting potential analysis of Jinghongshan-Eboliang area in Altunshan area[J].Contributions to Geology and Mineral Resources Research,33(01):23-30(in Chinese).
Mei Hualin,Yu Haifeng,Lu Songnian,Li Huimin,Li Shuan,Lin Yuanxian,Zuo Yicheng.1998.Archean tonalite in the Dunhuang,Gansu Province:Age from the U-Pb single zircon and Nd isotope[J].Progress in Precamrian Research,(02):41-45(in Chinese).
Meng Fancong,Zhang Jianxin,Xiang Zhenqun,Yu Shengyao,Li Jinping.2011.Evolution and formation of the Dunhuang group in NE Tarim basin,NW China:Evidence from detrital-zircon geochronology and Hf isotope[J].Acta Petrologica Sinica,27(1):59-76(in Chinese with English abstract).
Shi Mengyan,Hou Quanlin,Wu Chunming,Wang Hao,Chen Hongxu.2017.An analysis of the characteristics of the rock-structure association of the Dunhuang orogenic belt and their implications for tectonic setting[J].Geological Bulletin of China,36(2-3):238-250(in Chinese with English abstract).
Tang Hejun,Zhang Baolin,Ye Rong,Zhang Guoliang,Zhang Wenbin.2015.Geological characteristics and genesis of the Miaoping graphite deposit in Mian county of Shaanxi Province[J].Geology and Exploration,51(3):534-544(in Chinese with English abstract).
Wang Jingyong.2008.Identification of granitic orthogneiss of Dunhuang rock group in Xiadong area of Gansu Province and its significance[J].Gansu Geology,(3):22-26(in Chinese).
Wang Nan,Wu Cailai,Ma Changqian,Lei Min,Guo Wenfeng,Zhang Xi,Chen Hongjie.2016.Geochemistry,zircon U-Pb geochronology and Hf isotopic characteristics for Granites in southern Dunhuang block[J].Acta Petrologica Sinica,32(11):3753-3780(in Chinese with English abstract).
Wang Yong,Wang Bin,Chen Bailin,Wu Yu,Meng Lingtong,He Jiangtao,Chen Andong.2017.New evidence of 2.0-1.8 Ga granitic genesis Tarim plate belonging to Colombia supercontinent[J].Geology in China,44(2):407-408(in Chinese with English abstract).
Wang Zhongmei,Han Chunming,Su Benxun,Patrick Asamoah Sakyi,Sanjeewa Malaviarachchi,Ao Songjian,Wang Luojuan.2013.The metasedimentary rocks from the eastern margin of the Tarim Craton:Petrology,geochemistry,zircon U-Pb dating,Hf isotopes and tectonic implications[J].Lithos,179:120-136.
Wang Zhongmei,Han Chunming,Xiao Wenjiao,Wan Bo,Patrick Asamoah Sakyi,Ao Songjian,Zhang Ji'en,Song Dongfang.2014.Petrology and geochronology of Paleoproterozoic garnet-bearing amphibolites from the Dunhuang block,eastern Tarim Craton[J].Precambrian Research,255:163-180.
Xin Houtian,Liu Yongshun,Luo Zhaohua,Song Shunchang,Wang Shuqing.2013.The growth of Archean continental crust in Aqtashtagh area of southeast Tarim,China:Constraints from petrochemistry and chronology about Milan group and TTG-gneiss[J].Earth Science Frontiers,20(1):240-259(in Chinese with English abstract).
Xu Zhiqin,Yang Jingsui,Zhang Jianxin,Jiang Mei,Li Haibing,Cui Junwen.1999.A comparison between the tectonic units on the two sides of the Altun sinistral strike-slip fault and the mechanism of lithospheric shearing[J].Acta Geologica Sinica,(3):193-205(in Chinese).
Yan Lingya,Gao Shuxue,Chen Zhengguo,Jiao Lixiang,Sun Li,Liu Yanfei,Zhou Wen.2018.Metallogenic characteristics and metallogenic zoning of graphite deposits in China[J].Geology in China,45(3):421-440(in Chinese with English abstract).
Zhang Jianxin,Gong Jianghua,Yu Shengyao.2012.1.85Ga HP granulitefacies metamorphism in the Dunhuang block of the Tarim Craton,NW China:Evidence from U-Pb zircon dating of mafic granulites[J].Journal of the Geological Society,London,169(5):511-514.
Zhang Jianxin,Li Huaikun,Meng Fancong,Xiang Zhenqun,Yu Shengyao,Li Jinping.2011.Polyphase tectonothermal events recorded in“metamorphic basement”from the Altyn Tagh,the southeastern margin of the Tarim basin,western China:Constraint from U-Pb zircon geochronology[J].Acta Petrologica Sinica,27(1):23-46(in Chinese with English abstract).
Zhang Jianxin,Yu Shengyao,Gong Jianghua,Li Huaikun,Hou Kejun.2013.The latest Neoarchean-Paleoproterozoic evolution of the Dunhuang block,eastern Tarim craton,northwestern China:Evidence from zircon U-Pb dating and Hf isotopic analyses[J].Precambrian Research,226(1):21-42.
Zhang Tengfei.2015.The geochemical characteristics and deposit genesis analysis of Xiaochagou graphite deposit in Zhenping County of Henan Province[D].Beijing:China University of Geosciences(Beijing):1-70(in Chinese).
Zhao Yan,Diwu Chunrong,Sun Yong,Zhu Tao,Wang Hongliang.2013.Zircon geochronology and Lu-Hf isotope composition for Precambrian rocks of the Dunhuang complex in Shuixiakou area,Gansu Province[J].Acta Petrologica Sinica,29(05):1698-1712(in Chinese with English abstract).
Zhao Yan,Sun Yong,Yan Jianghao,Diwu Chunrong.2015.The ArcheanPaleoproterozoic crustal evolution in the Dunhuang region,NW China:Constraints from zircon U-Pb geochronology and in situ Hf isotopes[J].Precambrian Research,271:83-97.
Zhao Yan.2017.Composition and evolution of the Dunhuang orogenic belt[D].Xi'an:Northwest University:1-373(in Chinese).
Zong Keqing,Liu Yongsheng,Zhang Zeming,He Zhenyu,Hu Zhaochu,Guo Jingliang,Chen Kang.2013.The generation and evolution of Archean continental crust in the Dunhuang block,northeastern Tarim Craton,northwestern China[J].Precambrian Research,235:251-263.
Zhao Zhenming,Ji Wenhua,Li Wenming.2018.Metamorphic Genesis of Magnetite Quartzite with Iron Mineralization in the Dunhuang group of southern Beishan region[J].Geology and Exploration,54(4):689-701(in Chinese with English abstract).
白建科,陈隽璐,彭素霞.2017.新疆石墨资源特征及成矿规律[J].地质学报,91(12):2828-2840.
包伟航.2017.敦煌地块南缘前寒武纪及晚古生代大陆地壳演化[D].广州:中国科学院大学(中国科学院广州地球化学研究所):1-89.
甘肃省地质矿产局.1989甘肃省区域地质志[M].北京:地质出版社:1-692.
黄安.2017.内蒙古自治区查汗木胡鲁石墨矿矿床成因研究[D].北京:中国地质大学(北京):1-51.
姜高珍,李以科,王安建,杨轩,杨彪,马莉.2017.内蒙古乌拉特中旗大乌淀石墨矿成因特征分析[J].地学前缘,24(5):306-316.
李超,王登红,赵鸿,裴浩翔,李欣尉,周利敏,杜安道,屈文俊.2015.中国石墨矿床成矿规律概要[J].矿床地质,34(6):1223-1236.
李思远.2017.黑龙江省天然晶质石墨资源分布及矿床成因研究[D].北京:中国地质大学(北京):1-62.
梁帅.2015.华北典型晶质石墨矿床成因研究[D].阜新:辽宁工程技术大学:1-124.
路耀祖,徐加求.2018.阿尔金南缘金鸿山-俄博梁地区石墨矿化特征及找矿前景分析[J].地质找矿论丛,33(1):23-30.
梅华林,于海峰,陆松年,李惠民,李铨,林源贤,左义成.1998.甘肃敦煌太古宙英云闪长岩:单颗粒锆石U-Pb年龄和Nd同位素[J].前寒武纪研究进展,(2):41-45.
孟繁聪,张建新,相振群,于胜尧,李金平.2011.塔里木盆地东北缘敦煌群的形成和演化:锆石U-Pb年代学和Lu-Hf同位素证据[J].岩石学报,27(1):59-76
石梦岩,侯泉林,吴春明,王浩,陈泓旭.2017.敦煌造山带岩石-构造组合特征及其构造环境[J].地质通报,36(2-3):238-250.
汤贺军,张宝林,叶荣,张国梁,张文斌.2015.陕西勉县庙坪石墨矿床地质特征与成因初步探讨[J].地质与勘探,51(3):534-544.
王静永.2008.甘肃北山南带峡东地区敦煌岩群中花岗质正片麻岩的确认及其意义[J].甘肃地质,(03):22-26.
王楠,吴才来,马昌前,雷敏,郭文峰,张昕,陈红杰.2016.敦煌地块南部古生代花岗岩地球化学、锆石U-Pb定年及Hf同位素特征研究[J].岩石学报,32(12):3753-3780.
王永,王斌,陈柏林,吴玉,孟令通,何江涛,陈安东.2017.塔里木板块归属Colombia超大陆的新证据:来自北阿尔金地区2.0~1.8 Ga花岗质片麻岩体[J].中国地质,44(02):407-408.
辛后田,刘永顺,罗照华,宋顺昌,王树庆.2013.塔里木盆地东南缘阿克塔什塔格地区新太古代陆壳增生:米兰岩群和TTG片麻岩的地球化学及年代学约束[J].地学前缘,20(1):240-259
许志琴,杨经绥,张建新,姜枚,李海兵,崔军文.1999.阿尔金断裂两侧构造单元的对比及岩石圈剪切机制[J].地质学报,(03):193-205.
颜玲亚,高树学,陈正国,焦丽香,孙莉,刘艳飞,周雯.2018.中国石墨矿成矿特征及成矿区带划分[J].中国地质,45(03):421-440.
郁东良,王永刚,申大利.2016.柴达木盆地西北缘晶质石墨矿特征及找矿远景[J].现代矿业,32(09):179-181.
张建新,李怀坤,孟繁聪,相振群,于胜尧,李金平.2011.塔里木盆地东南缘(阿尔金山)“变质基底”记录的多期构造热事件:锆石U-Pb年代学的制约[J].岩石学报,27(1):23-46.
张腾飞.2015.河南省镇平县小岔沟石墨矿矿床地球化学特征及成因分析[D].北京:中国地质大学(北京):1-70.
赵燕,第五春荣,孙勇,朱涛,王洪亮.2013.甘肃敦煌水峡口地区前寒武纪岩石的锆石U-Pb年龄、Hf同位素组成及其地质意义[J].岩石学报,29(05):1698-1712.
赵燕.2017.敦煌造山带的构成及演化[D].西安:西北大学:1-373.
赵振明,计文化,李文明.2018.北山南部敦煌岩群铁矿化磁铁石英岩的变质成因[J].地质与勘探,54(04):689-701.