必须声明标量变量 "@Script_ID"。 青海矿床成矿系列探讨-《地球科学与环境学报》
|本期目录/Table of Contents|

[1]潘彤.青海矿床成矿系列探讨[J].地球科学与环境学报,2019,41(03):297-315.
 PAN Tong.Discussion on the Minerogenetic Series of Deposits in Qinghai, China[J].Journal of Earth Sciences and Environment,2019,41(03):297-315.
点击复制

青海矿床成矿系列探讨(PDF)
分享到:

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第41卷
期数:
2019年第03期
页码:
297-315
栏目:
基础地质与矿产地质
出版日期:
2019-05-15

文章信息/Info

Title:
Discussion on the Minerogenetic Series of Deposits in Qinghai, China
文章编号:
1672-6561(2019)03-0297-19
作者:
潘彤
(青海省地质矿产勘查开发局,青海 西宁 810001)
Author(s):
PAN Tong
(Bureau of Geological Exploration and Development of Qinghai Province, Xining 810001, Qinghai, China)
关键词:
矿床 成矿系列 矿产资源 成矿演化 成矿规律 成矿期 青海
Keywords:
deposit minerogenetic series mineral resource minerogenetic evolution minerogenetic regularity minerogenetic period Qinghai
分类号:
P612
DOI:
-
文献标志码:
A
摘要:
青海地质环境复杂,成矿条件优越,矿产资源相对丰富,构造上位于秦祁昆构造域和特提斯构造域的交接部位。在对青海已查明资源储量的石油、天然气、钾盐、石盐、Au、Fe、Cu、Ni、Pb-Zn、煤、石墨、大理岩等矿产为主的成矿地质条件进行总结的基础上,根据青海构造演化、岩石建造组合及矿产分布规律,运用成矿系列理论,初步划分出青海矿床33个成矿系列(组)、91个成矿亚系列、60个矿床式。主要成矿系列(组)有柴达木盆地新生代石油-K-Li-B-Mg-Sr-石盐-芒硝成矿系列、三江西北与中生代沉积-岩浆-构造作用有关的Cu-Pb-Zn-Ag-黄铁矿-水晶成矿系列组、东昆仑与华力西期—印支期旋回构造-岩浆-沉积作用有关的Fe-Cu-Ni-Co-Pb-Zn-Au-W-Sn-Nb-Ta成矿系列组、北祁连与加里东期岩浆作用有关的Cu-Pb-Zn-Au-石棉成矿系列、北祁连与前南华纪构造旋回岩浆作用有关的Fe-Pb-Zn-Au-硫铁矿-铬铁矿-石棉-蛇纹岩成矿系列。对每个成矿系列(组)及其分布特征等有关问题进行了讨论,重点对前南华纪、早古生代、晚古生代—早中生代、晚中生代、新生代5个成矿阶段的成矿系列特征进行了分析论述,建立了前南华纪古陆核形成、基底陆壳的板内成矿体系,早古生代板块体制成矿体系,晚古生代—早中生代古特提斯成矿体系,晚中生代新特提斯成矿体系,新生代高原隆升成矿体系。
Abstract:
Qinghai is relatively rich in mineral resources because of the complicated geological environment and favorable mineralization condition, which is located in the connection between Qinling-Qilian-Kunlun and Tethys tectonic domains. The metallogenic geological conditions of oil, natural gas, potash salt, rock salt, Au, Fe, Cu, Ni, Pb-Zn, coal, graphite and marble, etc., with identified resource reserves in Qinghai were summarized. The minerogenetic series of each mineralization unit in terms of tectonics, stratigraphic division, rock formation and mineral distribution were studied. Combined with the theory of the minerogenetic series, 33 minerogenetic series(groups), 91 minerogenetic subseries and 60 ore deposit types in Qinghai were initially divided. The main minerogenetic series(group)are as follow: the Cenozoic oil-K-Li-B-Mg-Sr-rock salt-glauber’s salt minerogenetic series in Qaidam Basin, the Mesozoic sedimentary-magmatic-tectonic-related Cu-Pb-Zn-Ag-pyrite-crystal minerogenetic series in the northwest of Sanjiang area, the Variscan-Indosinian tectonic-magmatic-sedimentary-related Fe-Cu-Ni-Co-Pb-Zn-Au-W-Sn-Nb-Ta minerogenetic series in East Kunlun, the Caledonian magmatism-related Cu-Pb-Zn-Au-asbestos minerogenetic series in North Qilian, and the Pre-Nanhua tectonic-magmatic-related Fe-Pb-Zn-Au-pyrite-chromite-asbestos-serpentine minerogenetic series in North Qilian. The five important minerogenetic periods including Pre-Nanhua, Early Paleozoic, Late Paleozoic-Early Mesozoic, Late Mesozoic and Cenozoic were discussed, and finally the framework of minerogenetic series in Qinghai was established. The intraplate minerogenetic system of basement continental crust related to the formation of Pre-Nanhua paleocentric core, Early Paleozoic plate tectonic regime minerogenetic system, Late Paleozoic-Early Mesozoic Paleo-Tethys minerogenetic system, Late Mesozoic Neo-Tethys minerogenetic system and Cenozoic plateau uplift minerogenetic system were established.

参考文献/References:

[1] 程裕淇,陈毓川,赵一鸣.初论矿床的成矿系列问题[J].地球学报,1979,1(1):32-58.
CHENG Yu-qi,CHEN Yu-chuan,ZHAO Yi-ming.Preliminary Discussion on the Problems of Minerogenetic Series of Mineral Deposits[J].Acta Geoscientica Sinica,1979,1(1):32-58.
[2] 程裕淇,陈毓川,赵一鸣,等.再论矿床的成矿系列问题[J].地球学报,1983,5(2):1-64.
CHENG Yu-qi,CHEN Yu-chuan,ZHAO Yi-ming,et al.Further Discussion on the Problems of Minerogenetic Series of Mineral Deposits[J].Acta Geoscientica Sinica,1983,5(2):1-64.
[3] 陈毓川,裴荣富,王登红.三论矿床的成矿系列问题[J].地质学报,2006,80(10):1501-1508.
CHEN Yu-chuan,PEI Rong-fu,WANG Deng-hong.On Minerogenetic(Metallogenetic)Series:The Third Discussion[J].Acta Geologica Sinica,2006,80(10):1501-1508.
[4] 潘 彤.柴达木盆地北缘Ⅳ级成矿单元划分[J].世界地质,2018,37(4):1137-1148.
PAN Tong.Classification of Level Ⅳ Metallogenic Units in Northern Qaidam Basin[J].Global Geology,2018,37(4):1137-1148.
[5] 潘 彤,孙丰月,李智民,等.青海省东昆仑钴矿成矿系列研究[M].北京:地质出版社,2005.
PAN Tong,SUN Feng-yue,LI Zhi-min,et al.Study on the Metallogenic Series of Cobalt Deposits in East Kunlun,Qinghai Province[M].Beijing:Geological Publishing House,2005.
[6] 潘 彤,王秉璋,李东生,等.青海东昆仑成矿环境、成矿规律与找矿方向[M].北京:地质出版社,2016.
PAN Tong,WANG Bing-zhang,LI Dong-sheng,et al.Study on the Metallogenic Environment,Metallogenic Regularities and Prospecting Direction in East Kunlun,Qinghai[M].Beijing:Geological Publishing House,2016.
[7] 杨生德,潘 彤.青海省矿产资源潜力评价研究报告[R].西宁:青海省地质矿产勘查开发局,2013.
YANG Sheng-de,PAN Tong.Report on Metallogenic Settings in Mineral Resources Potentiality Assesment in Qinghai Province[R].Xining:Bureau of Geological Exploration and Development of Qinghai Province,2013.
[8] 潘 彤,王福德.初论青海省金矿成矿系列[J].黄金科学技术,2018,26(4):423-430.
PAN Tong,WANG Fu-de.Preliminary Discussion on Minerogentic Series of Gold Deposits in Qinghai Province[J].Gold Science and Technology,2018,26(4):423-430.
[9] 王福德,李云平,贾妍慧.青海金矿成矿规律及找矿方向[J].地球科学与环境学报,2018,40(2):162-175.
WANG Fu-de,LI Yun-ping,JIA Yan-hui.Metallogenic Regularity and Prospecting Direction of Gold Deposits in Qinghai,China[J].Journal of Earth Sciences and Environment,2018,40(2):162-175.
[10] 张新虎,任丰寿,余 超,等.甘肃成矿系列研究及矿产勘查新突破[J].矿床地质,2015,34(6):1130-1140.
ZHANG Xin-hu,REN Feng-shou,YU Chao,et al.Breakthrough in Geological Prospecting Based on Study of Metallogenic Regularity[J].Mineral Depo-sits,2015,34(6):1130-1140.
[11] 董连慧,刘德权,唐延龄,等.试论新疆成矿体系与时空演化模式[J].矿床地质,2015,34(6):1107-1129.
DONG Lian-hui,LIU De-quan,TANG Yan-ling,et al.Five-era Metallogenic System of Mineral Deposits in Xinjiang and Its Spatial and Temporal Evolution Mode[J].Mineral Deposits,2015,34(6):1107-1129.
[12] 于学峰,张天祯,王 虹,等.山东省矿床成矿系列研究[J].矿床地质,2016,35(1):169-184.
YU Xue-feng,ZHANG Tian-zhen,WANG Hong,et al.A Study of Minerogenetic Series of Mineral Deposits in Shandong Province[J].Mineral Deposits,2016,35(1):169-184.
[13] 朱裕生,肖克炎,宋国耀,等.中国主要成矿区带成矿地质特征及矿床成矿谱系[M].北京:地质出版社,2007.
ZHU Yu-sheng,XIAO Ke-yan,SONG Guo-yao,et al.Geological Feature and Metallogenetic Pedigree of Ore Deposits in the Major Metallogenetic Regions Belts,China[M].Beijing:Geological Publishing House,2007.
[14] 潘桂棠,肖庆辉,陆松年,等.中国大地构造单元划分[J].中国地质,2009,36(1):1-28.
PAN Gui-tang,XIAO Qing-hui,LU Song-nian,et al.Division of Tectonic Stages and Tectonic Evolution in China[J].Geology in China,2009,36(1):1-28.
[15] 潘 彤.青海成矿单元划分[J].地球科学与环境学报,2017,39(1):16-33.
PAN Tong.Classification of Metallogenic Units in Qinghai,China[J].Journal of Earth Sciences and Environment,2017,39(1):16-33.
[16] 青海省国土资源厅.青海省2015年度矿产资源储量统计工作报告[R].西宁:青海省国土资源厅,2016.
Land and Resources Department of Qinghai Province.Report on Mineral Reserves Statistics of Qinghai Province in 2015[R].Xining:Land and Resources Department of Qinghai Province,2016.
[17] 陈毓川,王平安,秦克令,等.秦岭地区主要金属矿床成矿系列的划分及区域成矿规律探讨[J].矿床地质,1994,13(4):289-298.
CHEN Yu-chuan,WANG Ping-an,QIN Ke-ling,et al.Metallogenic Series of Main Ore Deposits and Regional Metallogeny in the Qinling Area[J].Mineral Deposits,1994,13(4):289-298.
[18] 陈毓川,常印佛,裴荣富,等.中国成矿体系与区域成矿评价[M].北京:地质出版社,2007.
CHEN Yu-chuan,CHANG Yin-fo,PEI Rong-fu,et al.Mineralization System and Evaluation of Regional Mineralization in China[M].Beijing:Geological Publishing House,2007.
[19] 沈保丰,杨春亮,翟安民,等.中国前寒武纪地壳演化与成矿[J].矿床地质,2004,23(增):78-89.
SHEN Bao-feng,YANG Chun-liang,ZHAI An-min,et al.Precambrian Crustal Evolution and Mineralization in China[J].Mineral Deposits,2004,23(S):78-89.
[20] 郭现轻,闫 臻,付长垒,等.青海南山“金水口岩群”的时代与构造属性研究[J].地质学报,2016,90(3):589-606.
GUO Xian-qing,YAN Zhen,FU Chang-lei,et al.Formation Age and Tectonic Attribute of Jinshuikou Group Complex in the Nanshan Area,Qinghai[J].Acta Geologica Sinica,2016,90(3):589-606.
[21] 青海省地质调查院.1:50 000尕牙合幅区域地质调查报告[R].西宁:青海省地质调查院,1998.
Qinghai Geological Survey Institute.Investigation Report of Gayahe Regional Geology(1:50 000)[R].Xining:Qinghai Geological Survey Institute,1998.
[22] 董国安,杨怀仁,杨宏仪,等.祁连地块前寒武纪基底锆石SHRIMP U-Pb年代学及其地质意义[J].科学通报,2007,52(13):1572-1585.
DONG Guo-an,YANG Huai-ren,YANG Hong-yi,et al.SHRIMP U-Pb Geochronology of the Zircons from the Precambrian Basement of the Qilian Block and Its Geological Significances[J].Chinese Science Bulletin,2007,52(13):1572-1585.
[23] 孟繁聪,田广阔,段雪鹏,等.东昆仑东段金水口石榴堇青石花岗岩成因:石榴子石证据[J].矿物岩石地球化学通报,2018,37(2):192-204.
MENG Fan-cong,TIAN Guang-kuo,DUAN Xue-peng,et al.Evidence from Garnet for Genesis of Garnet-cordierite-granite in the Jinshuikou Area,Eastern Segment of the East Kunlun Mountains[J].Bulletin of Minera-logy,Petrology and Geochemistry,2018,37(2):192-204.
[24] 钱 兵,张照伟,刘会文,等.柴达木西北缘古生代镁铁-超镁铁质岩体Cu-Ni成矿条件与找矿潜力分析[J].西北地质,2017,50(1):35-49.
QIAN Bing,ZHANG Zhao-wei,LIU Hui-wen,et al.Analysis on the Prospecting Potentiality and Cu-Ni Metallogenic Conditions of the Paleozoic Mafic-ultramafic in the Northwestern Margin of Qaidam Basin[J].Northwestern Geology,2017,50(1):35-49.
[25] 赖健清,鞠培姣,周 凤.青海省果洛龙洼金矿多因复成成矿作用[J].中国有色金属学报,2016,26(2):402-414.
LAI Jian-qing,JU Pei-jiao,ZHOU Feng.Polygenetic Compound Mineralization of Guoluolongwa Gold Deposit in Qinghai Province,China[J].The Chinese Journal of Nonferrous Metals,2016,26(2):402-414.
[26] 王国灿,王青海,简 平,等.东昆仑前寒武纪基底变质岩系的锆石SHRIMP年龄及其构造意义[J].地学前缘,2004,11(4):481-490.
WANG Guo-can,WANG Qing-hai,JIAN Ping,et al.Zircon SHRIMP Ages of Precambrian Metamorphic Basement Rocks and Their Tectonic Significance[J].Earth Science Frontiers,2004,11(4):481-490.
[27] 郭进京,赵凤清,李怀坤,等.中祁连东段湟源群的年代学新证据及其地质意义[J].中国区域地质,2000,19(1):26-31.
GUO Jin-jing,ZHAO Feng-qing,LI Huai-kun,et al.New Chronological Evidence of the Age of Huangyuan Group in the Eastern Segment of Mid-Qilian Massif and Its Geological Significance[J].Regional Geology of China,2000,19(1):26-31.
[28] 万渝生,许志琴,杨经绥,等.祁连造山带及邻区前寒武纪深变质基底的时代和组成[J].地质学报,2003,24(4):319-324.
WAN Yu-sheng,XU Zhi-qin,YANG Jing-sui,et al.Ages and Compositions of the Precambrian High-grade Basement of the Qilian Terrane and Its Adjacent Areas[J].Acta Geologica Sinica,2003,24(4):319-324.
[29] 张招崇,周美夫,PAUL T R,等.北祁连山西段熬油沟蛇绿岩SHRIMP分析结果及其地质意义[J].岩石学报,2001,17(2):222-226.
ZHANG Zhao-chong,ZHOU Mei-fu,PAUL T R,et al.SHRIMP Dating of the Aoyougou Ophiolite in the West Sector of the North Qilian Mountains and Its Geological Significance[J].Acta Petrologica Sinica,2001,17(2):222-226.
[30] 魏启荣,李德威,王国灿.东昆仑万保沟群火山岩岩石地球化学特征及其构造背景[J].矿物岩石,2007,27(1):97-106.
WEI Qi-rong,LI De-wei,WANG Guo-can.Geochemical Characteristics and Tectonic Setting of Volcanic Rocks from the Wanbaogou Group in East Kunlun Oro-genic Belt[J].Journal of Mineralogy and Petrology,2007,27(1):97-106.
[31] 张 强,丁清峰,宋 凯,等.东昆仑洪水河铁矿区狼牙山组千枚岩碎屑锆石U-Pb年龄、Hf同位素及其地质意义[J].吉林大学学报(地球科学版),2018,48(4):1085-1104.
ZHANG Qiang,DING Qing-feng,SONG Kai,et al.Detrital Zircon U-Pb Geochronology and Hf Isotope of Phyllite of Langyashan Formation in Hongshuihe Iron Ore District of Eastern Kunlun and Their Geological Significance[J].Journal of Jilin University(Earth Science Edition),2018,48(4):1085-1104.
[32] 何世平,李荣社,王 超,等.昌都地块宁多岩群形成时代研究:北羌塘基底存在的证据[J].地学前缘,2013,20(5):15-24.
HE Shi-ping,LI Rong-she,WANG Chao,et al.Research on the Formation Age of Ningduo Rock Group in Changdu Block:Evidence for the Existence of Basement in the North Qiangtang[J].Earth Science Frontiers,2013,20(5):15-24.
[33] 潘桂棠,陆松年,肖庆辉,等.中国大地构造阶段划分和演化[J].地学前缘,2016,23(6):1-23.
PAN Gui-tang,LU Song-nian,XIAO Qing-hui,et al.Division of Tectonic Stages and Tectonic Evolution in China[J].Earth Science Frontiers,2016,23(6):1-23.
[34] 夏祖春,夏林圻,徐学义.北祁连山元古宙末—寒武纪主动大陆裂谷火山作用[J].地球学报,1996,17(3):282-291.
XIA Zu-chun,XIA Lin-qi,XU Xue-yi.The Late Pro-terozoic-Cambrian Active Continental Rift Volcanism in Northern Qilian Mountains[J].Acta Geoscientica Sinica,1996,17(3):282-291.
[35] 青海省地质调查院.青海省1:500 000大地构造相图说明书[R].西宁:青海省地质调查院,2012.
Qinghai Geological Survey Institute.Manual on 1:500 000 Tectonic Map in Qinghai Province[R].Xining:Qinghai Geological Survey Institute,2012.
[36] 李怀坤,陆松年,王惠初,等.青海柴北缘新元古代超大陆裂解的地质记录:全吉群[J].地质调查与研究,2003,26(1):27-37.
LI Huai-kun,LU Song-nian,WANG Hui-chu,et al.Quanji Group:The Geological Record of Neoproterozoic Rift on the North Margin of the Qaidam Basin in Qinghai Province[J].Geological Survey and Research,2003,26(1):27-37.
[37] 王 超,李 猛,李荣社,等.青海柴达木盆地北缘全吉群内部存在区域性不整合[J].地质通报,2015,34(2):364-373.
WANG Chao,LI Meng,LI Rong-she,et al.Recognition of the Regional Unconformity in the Neoprotero-zoic Quanji Group on the North Margin of the Qaidam Basin in Qinghai Province[J].Geological Bulletin of China,2015,34(2):364-373.
[38] 青海省地质调查院.1:250 000库朗米其提幅区域地质调查报告[R].西宁:青海省地质调查院,2003.
Qinghai Geological Survey Institute.Geological Survey Report of 1:250 000 Kulangmiqiti Sheet[R].Xining:Qinghai Geological Survey Institute,2003.
[39] 刘懿馨,沙 鑫,马 蓁,等.北祁连西段双龙镁铁质—超镁铁质岩地球化学特征及构造意义[J].岩石学报,2018,34(2):383-397.
LIU Yi-xin,SHA Xin,MA Zhen,et al.Geochemical Characteristics and Tectonic Implication of the Shuang-long Mafic-ultramafic Rocks in Western Section of the North Qilian[J].Acta Petrologica Sinica,2018,34(2):383-397.
[40] 闫海卿,余吉远,李文渊,等.祁连造山带早古生代矿床成矿系列与演化[J].矿床地质,2004,23(增):137-142.
YAN Hai-qing,YU Ji-yuan,LI Wen-yuan,et al.Meta-llogenic Series and Evolution in Qilian Orogenic Belt in Early Paleozoic[J].Mineral Deposits,2004,23(S):137-142.
[41] 冯益民,何世平.祁连山及其邻区大地构造基本特征[J].西北地质科学,1995,16(1):92-103.
FENG Yi-min,HE Shi-ping.Basic Characteristics of Tectonics in the Qilian Mountains and Its Neighbourings[J].Northwestern Geoscience,1995,16(1):92-103.
[42] 潘裕生,方爱民.中国青藏高原特提斯的形成与演化[J].地质科学,2010,45(1):92-101.
PAN Yu-sheng,FANG Ai-min.Formation and Evolution of the Tethys in the Tibetan Plateau[J].Chinese Journal of Geology,2010,45(1):92-101.
[43] 姜春发,王宗赵,李锦轶.昆仑开合构造[M].北京:地质出版社,1992.
JIANG Chun-fa,WANG Zong-zhao,LI Jin-yi.Opening-closing Tectonics of Kunlun[M].Beijing:Geological Publishing House,1992.
[44] 张 旗.中国蛇绿岩研究中的几个问题[J].地质科学,1992(增):139-146.
ZHANG Qi.Some Problems on Ophiolite Study in China[J].Scientia Geologica Sinica,1992(S):139-146.
[45] 莫宣学,路凤香,沈上越,等.三江特提斯火山作用与成矿[M].北京:地质出版社,1993.
MO Xuan-xue,LU Feng-xiang,SHEN Shang-yue,et al.Volcanism and Metallogenesis of Sanjiang Tethy[M].Beijing:Geological Publishing House,1993.
[46] 罗中舒.板块构造与青藏高原煤田关系的探讨[J].煤炭学报,1980(2):34-43.
LUO Zhong-shu.Investigation on the Relationship Between Plate Tectonics and Coal Deposits in Qinghai-Xizang Plateau[J].Journal of China Coal Society,1980(2):34-43.
[47] 陈建平,郝金华.青海南部三江北段铜多金属成矿系统演化研究[J].西北地质,2012,45(1):236-243.
CHEN Jian-ping,HAO Jin-hua.Study on the Ore Forming System Evolution in Northern Sanjiang Meta-llogenic Belt,Qinghai Province[J].Northwestern Geo-logy,2012,45(1):236-243.
[48] 祁生胜.青海省大地构造单元划分与成矿作用特征[J].青海国土经略,2013(5):53-62.
QI Sheng-sheng.Tectonic Units Division of Qinghai Province and the Mineralization Characteristics[J].Management and Strategy of Qinghai Land and Resources,2013(5):53-62.
[49] 高小芬,林 晓,张智勇,等.青藏高原第四纪钾盐矿时空分布特征及成矿控制因素[J].地质通报,2013,32(1):186-194.
GAO Xiao-fen,LIN Xiao,ZHANG Zhi-yong,et al.Spatial-temporal Distribution Characteristics and Ore-controlling Factors of Quaternary Potash Deposits on the Tibetan Plateau[J].Geological Bulletin of China,2013,32(1):186-194.
[50] 侯增谦,杨竹森,徐文艺,等.青藏高原碰撞造山带:Ⅰ.主碰撞造山成矿作用[J].矿床地质,2006,25(4):337-358.
HOU Zeng-qian,YANG Zhu-sen,XU Wen-yi,et al.Metallogensis in the Tibetan Collisional Orogenic Belt:I.Mineralization in the Main-collisional Orogenic Setting[J].Mineral Deposits,2006,25(4):337-358.
[51] 侯增谦,潘桂棠,王安建,等.青藏高原碰撞造山带:Ⅱ.晚碰撞转换成矿作用[J].矿床地质,2006,25(5):521-533.
HOU Zeng-qian,PAN Gui-tang,WANG An-jian,et al.The Tibetan Collisional Orogenic Belt:Ⅱ.Metallo-genesis in Late-collisional Epoch[J].Mineral Deposits,2006,25(5):521-533.
[52] 侯增谦,曲晓明,杨竹森,等.青藏高原碰撞造山带:Ⅲ.后碰撞伸展成矿作用[J].矿床地质,2006,25(6): 629-651.
HOU Zeng-qian,QU Xiao-ming,YANG Zhu-sen,et al.Metallogenesis in Tibetan Collisional Orogenic Belt:Ⅲ.Mineralization in Post-collisional Extension Setting[J].Mineral Deposits,2006,25(6):629-651.
[53] 李德威.青藏高原及邻区三阶段构造演化与成矿演化[J].地球科学,2008,33(6):723-741.
LI De-wei.Three-stage Tectonic Evolution and Meta-llogenic Evolution in the Qinghai-Tibet Plateau and Its Adjacent Area[J].Earth Science,2008,33(6):723-741.
[54] 吴光大,葛肖虹,刘永江,等.柴达木盆地中、新生代构造演化及其对油气的控制[J].世界地质,2006,25(4):411-417.
WU Guang-da,GE Xiao-hong,LIU Yong-jiang,et al.Mesozoic-Cenozoic Structural Evolution in Qaidam Basin and Its Control on Hydrocarbon Occurrence[J].Global Geology,2006,25(4):411-417.
[55] 宋玉财,侯增谦,王贵仁,等.“三江”北段沱沱河地区的成矿规律与找矿方向[J].矿床地质,2015,34(1):1-20.
SONG Yu-cai,HOU Zeng-qian,WANG Gui-ren,et al.Metallogenic Regularity and Ore Exploration Targeting in Tuotuohe Area,Northern Sanjiang Orogenic Belt[J].Mineral Deposits,2015,34(1):1-20.
[56] 马鸿文.西藏玉龙斑岩铜矿带花岗岩类与成矿[M].武汉:中国地质大学出版社,1990.
MA Hong-wen.Petrology and Mineralization of Granites in Yulong Porphyry Copper Belt,Tibet[M].Wuhan:China University of Geosciences Press,1990.
[57] 魏新俊,姜继学.柴达木盆地第四纪盐湖演化[J].地质学报,1993,67(3):255-265.
WEI Xin-jun,JIANG Ji-xue.The Evolution of Quaternary Salt Lake in the Qaidam Basin[J].Acta Geologica Sinica,1993,67(3):255-265.
[58] 徐凤银,尹成明,巩庆林,等.柴达木盆地中、新生代构造演化及其对油气的控制[J].世界地质,2006,25(4):9-17.
XU Feng-yin,YIN Cheng-ming,GONG Qing-lin,et al.Mesozoic-Cenozoic Structural Evolution in Qaidam Basin and Its Control over Oil and Gas[J].Global Geo-logy,2006,25(4):9-17.
[59] 刘 林,宋 哲,宋宪生,等.柴达木盆地北缘中、新生代地质构造演化与砂岩型铀成矿关系[J].东华理工大学学报(自然科学版),2008,31(4):306-312.
LIU Lin,SONG Zhe,SONG Xian-sheng,et al.Study on the Relationships Between the Structural Evolution and Sandstone-type Uranium Minerallization in Mesozoic Era and Cenozoic Era in the Northern of Qaidam Basin[J].Journal of East China Institute of Technology(Science and Technology Edition),2008,31(4):306-312.
[60] 邹依林,李蒙文,葛良胜,等.西藏崩纳藏布砂金矿地质特征及找矿方向[J].黄金地质,2002,8(2):8-14.
ZOU Yi-lin,LI Meng-wen,GE Liang-sheng,et al.Geo-logical Features of Gold Placer and Prospecting Guide in Bengnazangbu,Tibet[J].Gold Geology,2002,8(2):8-14.

相似文献/References:

备注/Memo

备注/Memo:
收稿日期:2018-10-11; 修回日期:2019-01-02 投稿网址:http://jese.chd.edu.cn/
基金项目:中国地质调查局地质调查项目(DD20160346); 青海省重大科技专项项目(2016-SF-A3)
作者简介:潘 彤(1966-),男,青海乐都人,教授级高级工程师,理学博士,E-mail:pant66@163.com。
更新日期/Last Update: 2019-05-20