四川阿坝州党坝超大型锂辉石矿床成矿规律及深部和外围找矿方向

王子平; 刘善宝; 马圣钞; 刘丽君; 代鸿章; 郭唯明; 陈备战; 王子平; 刘善宝; 马圣钞; 刘丽君; 代鸿章; 郭唯明; 陈备战

doi:10.3799/dqkx.2018.604

[1]

Černý, P., 1991a.Fertile Granites of Precambrian Rare-Element Pegmatite Fields:Is Geochemistry Controlled by Tectonic Setting or Source Lithologies? Precambrian Research, 51(1-4):429-468.https://doi.org/10.1016/0301-9268(91)90111-m doi: 10.1016/0301-9268(91)90111-M

[2]

Černý, P., 1991b.Rare-Element Granite Pegmatites:Part Ⅱ.Regional to Global Environments and Petrogenesis.Geoscience Canada, 18(2):68-81. http://www.sciepub.com/reference/183976

[3]

Chen, Y.C., Ye, Q.T., Wang, J.B., et al., 2003.Geology, Metallogenic Regularity and Technical and Economic Evaluation of Ore Deposits in Altai Metallogenic Belt, Xinjiang, China.Geological Press, Beijing, 453(in Chinese).

[4]

Fei, G.C., Yuan, T.J., Tang, W.C., et al., 2014.Simple Division on Pegmatite-Type Rare Metal Deposits Ore-Bearing Pegmatites in Keeryin, Sichuan.Mineral Deposits, 33(Suppl.):187-188 (in Chinese). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXJZ200404019.htm

[5]

Gu, C.H., 2014.Metallogenic Regularity of Spodumene Deposits in the Closely Spaced Pegmatite Area in the Southeastern Keeryin Pegmatite Field, Sichuan Province.Contributions to Geology and Mineral Resources Research, 29(1):59-65 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzzklc201401007

[6]

Guo, C.L., Chen, Y.C., Li, C.B., et al., 2011.Zircon SHRIMP U-Pb Dating, Geochemistry, Sr-Nd Isotopic Analysis of the Late Jurassic Granitoids in the Jiulongnao W-Sn-Pb-Zn Ore-Concentrated Areas in Jiangxi Province and Their Geological Significance.Acta Geologica Sinica, 85(7):1188-1205 (in Chinese with English abstract). doi: 10.1007%2Fs11430-013-4610-9

[7]

Hao, X.F., Fu, X.F., Liang, B., et al., 2015.Formation Ages of Granite and XO3 Pegmatite Vein in Jiajika, Western Sichuan, and Their Geological Significance.Mineral Deposits, 34(6):1199-1208 (in Chinese with English abstract). http://industry.wanfangdata.com.cn/dl/Detail/Periodical?id=Periodical_kcdz201506009

[8]

Li, J.K., Wang, D.H., 2007.Mineralizing Mechanism and Continental Geodynamics of Typical Pegmatie Deposits in Western Sichuan, China.Atomic Energy Press, Beijing, 1-20 (in Chinese).

[9]

Li, J.K., Wang, D.H., Fu, X.F., 2006.⁴⁰Ar/³⁹Ar Ages of the Keeryin Pegmatite Type Rare Metal Deposit, Western Sichuan, and Its Tectonic Significances.Acta Geologica Sinica, 80(6):843-848(in Chinese with English abstract). https://www.researchgate.net/publication/279017142_Cassiterite_U-Pb_and_muscovite_Ar-40-Ar-39_age_constraints_on_the_timing_of_mineralization_in_the_Xuebaoding_Sn-W-Be_deposit_western_China

[10]

Liao, Y.A., Yao, X.L., 1992.Evolution Feature and Minerogenetic Relations Peraluminous Granites from Jinchuan, Western Sichuan.Mineralogy and Petrology, 12(1):12-22 (in Chinese with English abstract). http://www.sciencedirect.com/science/article/pii/S1342937X16304750

[11]

Luo, D., 2017.Spodumene Ore Deposit Geological Characteristics Analysis in Dangba, Barkam, Sichuan Province.Sichuan Nonferrous Metals, (1):24-27 (in Chinese with English abstract). http://industry.wanfangdata.com.cn/dl/Detail/Periodical?id=Periodical_scysjs201504010

[12]

Pang, B., Gu, C.H., Li, L.B., et al., 2015.Geological Characteristics and Genesis of the Spodumene Deposit in Dangba, Barkam, Sichuan Province.Sichuan Nonferrous Metals, (4):31-34 (in Chinese with English abstract). http://industry.wanfangdata.com.cn/dl/Detail/Periodical?id=Periodical_scysjs201504010

[13]

Pang, B., Luo, W., Li, J., 2014.Geological Features of Dangba Spodumene Deposit, in Maerkang, Sichuan.Mineral Deposits, 33(Suppl.):245-246 (in Chinese). http://www.sciencedirect.com/science/article/pii/S0169136816301780

[14]

Rao, K.Y., 2016.The Geological Characteristics and Ore Exploration Targeting of Dilaqiu Lithium Deposit in Maerkang County, Sichuan Provice.Sichuan Nonferrous Metals, (1):54-57 (in Chinese with English abstract).

[15]

Shi, Z.L., Zhang, H.F., Cai, H.M., 2009.Petrogenesis of Strongly Peraluminous Granites in Markan Area, Songpan Fold Belt and Its Tectonic Implication.Earth Science, 34(4):569-584 (in Chinese with English abstract). http://www.earth-science.net/WebPage/Article.aspx?id=1861

[16]

Sichuan Bureau of Geology and Mineral Resources, Maerkang Jinxin Mining Ltd., 2015. General Exploration and Resource Reserve Verification Report on Lithium Ores in Dangba Minging, Maerkang County, Sichuan. Sichuan Bureau of Geology and Mineral Resources, Chengdu(in Chinese).

[17]

Tang, G.F., Wu, S.X., 1984.Geological Study on Jiajika Granitic Pegmatite Lithium Deposits in Kangding County, Sichuan.Geological Publishing House, Beijing(in Chinese).

[18]

Wang, D.H., Li, J., K., Fu, X.F., 2005.⁴⁰Ar/³⁹Ar Dating for the Jiajika Pegmatite-Type Rare Metal Deposit in Western Sichuan and Its Significance.Geochimica, 34(6):541-547 (in Chinese with English abstract). https://es.scribd.com/document/342746138/Data-Sess07

[19]

Wang, D.H., Liu, L.J., Hou, J.L., et al., 2017.A Preliminary Review of the Application of "Five Levels+Basement" Model for Jiajika-Style Rare Metal Deposits.Earth Science Frontiers, 24(5):1-7 (in Chinese with English abstract). http://www.sciencedirect.com/science/article/pii/088329279290002K

[20]

Wang, L.K., Huang, Z.L., 2002.Liquid Separation and Experiment of Li-F Granite.Science Press, Beijing, 280(in Chinese).

[21]

Zhao, Y. J., 2007. Mesozic Granitoids in Eastern Songpan-Ganze: Geochemistry, Petrogenesis and Tectonic Implications (Dissertation). Graduate School of Chinese Academy of Sciences, Guangzhou(in Chinese).

[22]

陈毓川, 叶庆同, 王京彬, 等, 2003.中国新疆阿尔泰成矿带矿床地质、成矿规律与技术经济评价.北京:地质出版社, 453.

[23]

费光春, 袁天晶, 唐文春, 等, 2014.西川西可尔因伟晶岩型稀有金属矿床含矿伟晶岩分类浅析.矿床地质, 33(增刊):187-188. http://www.cnki.com.cn/Article/CJFDTotal-KCDZ2014S1096.htm

[24]

古城会, 2014.四川省可尔因伟晶岩田东南密集区锂辉石矿床成矿规律.地质找矿论丛, 29(1):59-65. doi: 10.6053/j.issn.1001-1412.2014.01.007

[25]

郭春丽, 陈毓川, 黎传标, 等, 2011.赣南晚侏罗世九龙脑钨锡铅锌矿集区不同成矿类型花岗岩年龄、地球化学特征对比及其地质意义.地质学报, 85(7):1188-1205. http://www.oalib.com/paper/4875691

[26]

郝雪峰, 付小方, 梁斌, 等, 2015.川西甲基卡花岗岩和新三号矿脉的形成时代及意义.矿床地质, 34(6):1199-1208. http://industry.wanfangdata.com.cn/dl/Detail/Periodical?id=Periodical_kcdz201506009

[27]

李建康, 王登红, 2007.川西伟晶岩型矿床的形成机制及大陆动力学背景.北京:原子能出版社, 1-20.

[28]

李建康, 王登红, 付小方, 2006.川西可尔因伟晶岩型稀有金属矿床的⁴⁰Ar/³⁹Ar年代及其构造意义.地质学报, 80(6):843-848. https://www.wenkuxiazai.com/word/4b676031a32d7375a417804b-1.doc

[29]

廖远安, 姚学良, 1992.金川一过铝多阶段花岗岩体演化特征及其与成矿关系.矿物岩石, 12(1):12-22. http://mall.cnki.net/magazine/Article/KWYS199201007.htm

[30]

罗典, 2017.四川省马尔康党坝锂辉石矿床地质特征分析.四川有色金属, (1):24-27. http://www.cnki.com.cn/Article/CJFDTotal-KCDZ2014S1125.htm

[31]

庞博, 古城会, 李良波, 等, 2015.四川省马尔康党坝锂辉石矿床地质特征及成因研究.四川有色金属, (4):31-34. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=scysjs201504010

[32]

庞博, 罗伟, 李剑, 2014.四川省马尔康党坝锂辉石矿床地质特征.矿床地质, 33(增刊):245-246. http://www.cnki.com.cn/Article/CJFDTotal-KCDZ2014S1125.htm

[33]

饶魁元, 2016.四川马尔康地拉秋锂矿床地质特征及找矿方向.四川有色金属, (1):54-57. http://www.cqvip.com/QK/92704X/201601/668343195.html

[34]

时章亮, 张宏飞, 蔡宏明, 2009.松潘造山带马尔康强过铝质花岗岩的成因及其构造意义.地球科学, 34(4):569-584. http://www.earth-science.net/WebPage/Article.aspx?id=1861

[35]

四川省地质矿产勘查开发局化探队, 马尔康金鑫矿业有限公司, 2015. 四川省马尔康县党坝矿区锂矿补充详查及资源储量核实报告. 成都: 四川省地质矿产勘查局.

[36]

唐国凡, 吴盛先, 1984.四川省康定县甲基卡花岗伟晶岩锂矿床地质研究报告.北京, 地质出版社.

[37]

王登红, 李建康, 付小方, 2005.四川甲基卡伟晶岩型稀有金属矿床的成矿时代及其意义.地球化学, 34(6):541-547. http://www.cnki.com.cn/Article/CJFDTOTAL-DQHX200506001.htm

[38]

王登红, 刘丽君, 侯江龙, 等, 2017.初论甲基卡式稀有金属矿床"五层楼+地下室"勘查模型.地学前缘, 24(5):1-7. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dxqy201705002&dbname=CJFD&dbcode=CJFQ

[39]

王联魁, 黄智龙, 2000.Li-F花岗岩液态分离与实验.北京:科学出版社, 280.

[40]

赵永久, 2007. 松潘-甘孜东部中生代中酸性侵入体的地球化学特征、岩石成因及构造意义(博士学位论文). 广州: 中国科学院研究生院.