新疆阿尔金西段瓦石峡南锂铍稀有金属矿成矿背景与勘查进展

doi:10.19388/j.zgdzdc.2024.03.03

Abstract
Figure/Table
References
Related Citation (6)

Download: PDF (5627 KB) HTML (1 KB)
Export: BibTeX | EndNote (RIS)

Abstract Rare metal minerals such as lithium and beryllium are important strategic mineral resources. In recent years, several rare metal pegmatite-type deposits have been discovered in Altyn area, which have emerged as a new rare metal metallogenic belt, but with relatively low investigation and research level. Through the discussion of the metallogenic dynamic background of the Altyn orogenic belt, the authors concluded that the rare metal metallogenesis in the Altyn orogenic belt covered many different tectonic evolution stages of the orogenic movement, indicating good metallogenic conditions for rare metals and great prospecting potential. The southern Waishixia lithium-beryllium rare metal deposit located in the western Altyn Tagh has a large prospect, based on the exploration and evaluation of this deposit. The lithium-beryllium rare metal ore body in the southern Washixia mainly occurs in the pegmatite veins of greenschist facies and amphibolite facies metamorphic rock series, and the deposit type is granite-pegmatite type rare metal deposit. According to the existing exploration results, the inferred rare metal resources of this deposit have reached the scale of medium and above, and there is still a great space for increasing storage in the deep and peripheral areas with the progress of exploration. The research results are of great reference significance to the deposit search of similar types in the Altyn orogenic belt.

Key words： Altyn Tagh the southern Washixia lithium-beryllium rare metal deposit granite-pegmatite type rare metal deposit mineralization dynamic background prospecting potential

Received: 14 March 2024

ZTFLH:

P618.6

	Service

	E-mail this article
	Add to my bookshelf
	Add to citation manager
	E-mail Alert
	RSS
	Articles by authors
	ZHANG Peng
	LIU Bao
	YANG Xiaofei
	LUO xintao
	DENG Langjiang
	FAN Zichun
	LIU Xingzhong
	CHEN Jianzhong
	LIU Shanbao
	WANG Denghong
	DAI Hongzhang

Cite this article:

ZHANG Peng,LIU Bao,YANG Xiaofei, et al. Metallogenic background and exploration progress of the southern Waishixia lithium-beryllium rare metal deposit in the western Altyn Tagh of Xinjiang Province[J]. , 2024, 11(3): 17-24.

URL:

http://journal25.magtechjournal.com/Jwk_dzdc/EN/10.19388/j.zgdzdc.2024.03.03 OR http://journal25.magtechjournal.com/Jwk_dzdc/EN/Y2024/V11/I3/17

[1] 张朋,王敬国,刘兴忠,等.阿尔金地区伟晶岩型稀有金属矿勘查进展及找矿前景分析[C]//第十届全国成矿理论与找矿方法学术讨论会论文摘要集.西安:中国矿物岩石地球化学学会矿床地球化学专业委员会,2023:87-88.
Zhang P,Wang J G,Liu X Z,et al.Exploration progress and prospecting prospect analysis of pegmatitic rare metal deposits in Altun area[C]//Abstracts of the 10th National Metallogenic Theory and Prospecting Method Symposium.Xi'an:Chinese Society for Mineralogy Petrology and Geochemistry,2023:87-88.
[2] 徐兴旺,李杭,石福品,等.阿尔金中段吐格曼地区花岗伟晶岩型稀有金属成矿特征与找矿预测[J].岩石学报,2019,35(11):3303-3316.
Xu X W,Li H,Shi F P,et al.Metallogenic characteristics and prospecting of granitic pegmatite-type rare metal deposits in Tugeman area,the middle part of Altyn Tagh[J].Acta Petrologica Sinica,2019,35(11):3303-3316.
[3] 杨智全,李磊,王超.新疆若羌县吐格曼稀有金属矿地质特征及找矿标志初探[J].中国金属通报,2020(1):38-39.
Yang Z Q,Li L,Wang C.A preliminary study on the geological characteristics and prospecting signs of Tugeman rare metal deposits in Ruoqiang County,Xinjiang[J].China Metal Bulletin,2020(1):38-39.
[4] 李杭,洪涛,杨智全,等.阿尔金中段吐格曼北花岗伟晶岩型锂铍矿床多阶段岩浆-成矿作用[J].岩石学报,2022,38(10):3085-3103.
Li H,Hong T,Yang Z Q,et al.Multi-stage magmatism-mineralization and tectonic setting of the North Tugeman granitic pegmatite lithium-beryllium deposit in the middle of Altyn Tagh[J].Acta Petrologica Sinica,2022,38(10):3085-3103.
[5] 代鸿章,刘善宝,王登红,等.新疆阿尔金稀有金属成矿带探获首例工业规模砂锂沟锂矿[J].中国地质,2023,50(4):1283-1284.
Dai H Z,Liu S B,Wang D H,et al.The first industrial scale Shaligou lithium deposit was discovered in Altun rare metal metallogenic belt,Xinjiang[J].Geology in China,2023,50(4):1283-1284.
[6] 吴益平,张连昌,袁波,等.新疆阿尔金地区卡尔恰尔超大型萤石矿床地质特征及成因[J].地球科学与环境学报,2021,43(6):962-977.
Wu Y P,Zhang L C,Yuan B,et al.Geological characteristics and genesis of the super-large kalqiar fluorite deposit in Altyn Tagh Area of Xinjiang,China[J].Journal of Earth Sciences and Environment,2021,43(6):962-977.
[7] 河南省地矿局第二地质勘査院.新疆阿尔金北缘拜什托格拉克一带1∶5万三幅区域地质矿产调査报告[R].2018:1-200.
Henan Provincial Bureau of Geology and Mineral Resources Second Geological Exploration Institute.Three 1∶50 000 Regional Geological and Mineral Survey Reports on the Northern Edge of Altun,Xinjiang in the Baishtograk area[R].2018:1-200.
[8] 董顺利,李忠,高剑,等.阿尔金-祁连-昆仑造山带早古生代构造格架及结晶岩年代学研究进展[J].地质论评,2013,59(4):731-746.
Dong S L,Li Z,Gao J,et al.Progress of studies on Early Paleozoic tectonic framework and crystalline rock geochronology in Altun-Qilian-Kunlun orogen[J].Geological Review,2013,59(4):731-746.
[9] Dai S,Dai W,Zhao Z B,et al.Timing,displacement and growth pattern of the Altyn Tagh fault:a review[J].Acta Geologica Sinica (English Edition),2017,91(2):669-687.
[10] 曾忠诚,边小卫,赵江林,等.阿尔金南缘冰沟南组火山岩锆石U-Pb年龄及其前寒武纪构造演化意义[J].地质论评,2019,65(1):103-118.
Zeng Z C,Bian X W,Zhao J L,et al.U-Pb geochronology of zircons from the volcanic rocks in bingounan formation,southern Altyn Tagh:implication for the precambrian tectonic evolution[J].Geological Review,2019,65(1):103-118.
[11] 何鹏,杨睿娜,陈培伟,等.阿尔金北缘尧勒萨依片麻岩锆石LA-ICP-MS U-Pb年龄、地球化学特征及其地质意义[J].地质论评,2021,67(3):803-815.
He P,Yang R N,Chen P W,et al.Zircon LA-ICP-MS U-Pb ages,geochemical features and their geological implications of Yaolesayi gneiss in north Altyn Tagh[J].Geological Review,2021,67(3):803-815.
[12] 何鹏,芦西战,杨睿娜,等.阿尔金北缘尧勒萨依河口I型花岗岩岩石地球化学、锆石U-Pb年代学研究[J].矿产勘查,2020,11(9):1822-1830.
He P,Lu X Z,Yang R N,et al.Petrogeochemistry,zircon U-Pb chronology of Ⅰ type granite from Yaolesayi estuary,northern Altun[J].Mineral Exploration,2020,11(9):1822-1830.
[13] 校培喜,高晓峰,胡云绪,等.阿尔金—东昆仑西段成矿带基础地质综合研究报告[R].西安:中国地质调查局西安地质调查中心,2012.
Xiao P X,Gao X F,Hu Y X,et al.Comprehensive research report on basic geology of Altyn Tagh-western section of east Kunlun metallogenic belt[R].Xi'an:China Geological Survey Xi'an Geological Survey Center,2012.
[14] 冯京,朱志新,赵同阳,等.新疆大地构造单元划分及成矿作用[J].中国地质,2022,49(4):1154-1178.
Feng J,Zhu Z X,Zhao T Y,et al.Subdivision of tectonic units and its metallogenesis in Xinjiang[J].Geology in China,2022,49(4):1154-1178.
[15] 何鹏. 新疆阿尔金北缘拜什托格拉克一带1∶5万三幅区域地质矿产调查新进展[J].中国矿业,2021,30(S1):255-259.
He P.New achievements on regional geological survey of three 1∶50 000 sheets of Bextograk in north Altyn-Tagh,Xinjiang[J].China Mining Magazine,2021,30(S1):255-259.
[16] 涂其军,李建康,王刚,等.中国西部主要伟晶岩型锂辉石矿床成矿作用对比及找矿前景[J].中国地质调查,2019,6(6):35-47.
Tu Q J,Li J K,Wang G,et al.Mineralization comparisons of the major pegmatite type spodumene deposits and their prospecting potential in West China[J].Geological Survey of China,2019,6(6):35-47.
[17] 王成辉,王登红,刘善宝,等.战略新兴矿产调查工程进展与主要成果[J].中国地质调查,2022,9(5):1-14.
Wang C H,Wang D H,Liu S B,et al.Progresses and main achievements on strategic emerging minerals survey project[J].Geological Survey of China,2022,9(5):1-14.
[18] 车自成,刘良,刘洪福,等.阿尔金山地区高压变质泥质岩石的发现及其产出环境[J].科学通报,1995,40(14):1298-1300.
Che Z C,Liu L,Liu H F,et al.Discovery of high-pressure metamorphic argillaceous rocks in the Altun Mountains and their production environment[J].Chinese Science Bulletin,1995,40(14):1298-1300.
[19] 许志琴,杨经绥,张建新,等.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,1999,73(3):193-205.
Xu Z Q,Yang J S,Zhang J X,et al.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,1999,73(3):193-205.
[20] 陈柏林,蒋荣宝,李丽,等.阿尔金山东段喀腊大湾地区铁矿带的发现及其意义[J].地球学报,2009,30(2):143-154.
Chen B L,Jiang R L,Li L,et al.Discovery of iron ore zones in the Kaladawan area within the eastern part of the Altun Mountains and its significance[J].Acta Geoscientica Sinica,2009,30(2):143-154.
[21] 陈柏林,祁万修,崔玲玲,等.阿尔金北缘喀腊达坂火山岩型铅锌矿床研究[J].地质学报,2017,91(8):1818-1835.
Chen B L,Qi W X,Cui L L,et al.The Kaladaban volcanogenic massive sulfide-type Pb-Zn deposit in northern Altun Mountains,NW China[J].Acta Geologica Sinica,2017,91(8):1818-1835.
[22] 乔耿彪,杨合群,杜玮,等.阿尔金成矿带成矿单元划分及成矿系列探讨[J].西北地质,2014,47(04):209-220.
Qiao G B,Yang H Q,Du W,et al.Discussion on metallogenic series and metallogenic unit division in Altun metallogenic belt[J].Northwestern Geology,2014,47(4):209-220.
[23] 王岩,邢树文,肖克炎.西昆仑-阿尔金Fe-Pb-Zn-Au-稀有金属成矿带成矿特征及资源潜力[J].地质学报,2016,90(7):1353-1363.
Wang Y,Xing S W,Xiao K Y.Metallgoenic features and resource potential of the west Kunlun to Altun Fe-Pb-Zn-Au-rare metals metallogenic belt[J].Acta Geologica Sinica,2016,90(7):1353-1363.
[24] 陈柏林,孟令通.阿尔金喀腊大湾铁矿田褶皱构造特征及找矿意义[J].大地构造与成矿学,2018,42(1):32-49.
Chen B L,Meng L T.Characteristics of folds in the Kaladawan Iron Orefield,Altun Mountains,northwestern China and its prospecting implication[J].Geotectonica et Metallogenia,2018,42(1):32-49.
[25] 张辉善,李艳广,全守村,等.阿尔金喀腊达坂铅锌矿床金属硫化物元素地球化学特征及其对成矿作用的制约[J].岩石学报,2018,34(8):2295-2311.
Zhang H S,Li Y G,Quan S C,et al.Geochemical characteristics of metallic sulfides from the Kaladaban deposit in Xinjiang and its implications for Pb-Zn ore-forming mechanism[J].Acta Petrologica Sinica,2018,34(8):2295-2311.
[26] 徐兴旺,洪涛,李杭,等.初论高温花岗岩-伟晶岩锂铍成矿系统:以阿尔金中段地区为例[J].岩石学报,2020,36(12):3572-3592.
Xu X W,Hong T,Li H,et al.Concept of high-temperature granite-pegmatite Li-Be metallogenic system with a primary study in the middle Altyn-Tagh[J].Acta Petrologica Sinica,2020,36(12):3572-3592.
[27] 李杭,洪涛,杨智全,等.稀有金属花岗伟晶岩锆石、锡石与铌钽铁矿U-Pb和白云母⁴⁰Ar/³⁹Ar测年对比研究——以阿尔金中段吐格曼北锂铍矿床为例[J].岩石学报,2020,36(9):2869-2892.
Li H,Hong T,Yang Z Q,et al.Comparative studying on zircon,cassiterite and coltan U-Pb dating and ⁴⁰Ar/³⁹Ar dating of muscovite rare-metal granitic pegmatites:A case study of the northern Tugeman lithium-beryllium deposit in the middle of Altyn Tagh[J].Acta Petrologica Sinica,2020,36(9):2869-2892.
[28] 张焕,何鹏,芦西战,等.阿尔金北缘瓦石峡南部稀有金属、稀土矿点的发现及意义[J].现代矿业,2022(1):34-36,87.
Zhang H,He P,Lu X Z,et al.Discovery and significance of rare and rare earth metal deposits in the south of Washixia,northern margin of Altun[J].Modern Mining,2022(1):34-36,87.
[29] 杨文强,刘良,丁海波,等.南阿尔金迪木那里克花岗岩地球化学、锆石U-Pb年代学与Hf同位素特征及其构造地质意义[J].岩石学报,2012,28(12):4139-4150.
Yang W Q,Liu L,Ding H B,et al.Geochemistry,geochronology and zircon Hf isotopes of the Dimunalike granite in South Altyn Tagn and its geological significance[J].Acta Petrologica Sinica,2012,28(12):4139-4150.
[30] 刘良,康磊,曹玉亭,等.南阿尔金早古生代俯冲碰撞过程中的花岗质岩浆作用[J].中国科学:地球科学,2015,45(8):1126-1137.
Liu L,Kang L,Cao Y T,et al.Early Paleozoic granitic magmatism related to the processes from subduction to collision in south Altyn,NW China[J].Science China:Earth Sciences,2015,58(9):1513-1522.
[31] 吴才来,郜源红,雷敏,等.南阿尔金茫崖地区花岗岩类锆石SHRIMP U-Pb定年、Lu-Hf同位素特征及岩石成因[J].岩石学报,2014,30(8):2297-2323.
Wu C L,Gao Y H,Lei M,et al.Zircon SHRIMP U-Pb dating,Lu-Hf isotopic characteristics and petrogenesis of the Palaeozoic granites in Mangya area,southern Altun,NW China[J].Acta Petrologica Sinica,2014,30(8):2297-2323.
[32] 吴锁平,吴才来,陈其龙.阿尔金断裂南侧吐拉铝质A型花岗岩的特征及构造环境[J].地质通报,2007,26(10):1385-1392.
Wu S P,Wu C L,Chen Q L.Characteristics and tectonic setting of the Tula aluminous A-type granite at the south side of the Altyn Tagh fault,NW China[J].Geological Bulletin of China,2007,26(10):1385-1392.
[33] Harris N B W,Pearce J A,Tindle A G.Geochemical Characteristics of Collision-Zone Magmatism[M]//Coward M P,Ries A C.Collision Tectonics.London:The Geological Society by Blackwell Scientific Publications,1986,19:67-81
[34] Pitcher W S.The Nature and Origin of Granite[M].2nd ed.London:Springer Dordrecht,1997,1-387.
[35] Barbarin B.A review of the relationships between granitoid types,their origins and their geodynamic environments[J].Lithos,1999,46(3):605-626
[36] 吴福元,刘志超,刘小驰,等.喜马拉雅淡色花岗岩[J].岩石学报,2015,31(1):1-36.
Wu F Y,Liu Z C,Liu X C,et al.Himalayan leucogranite:Petrogenesis and implications to orogenesis and plateau uplift[J].Acta Petrologica Sinica,2015,31(1):1-36.
[37] 新疆维吾尔自治区地质矿产勘查开发局第三地质大队.新疆若羌县瓦石峡南锂铍矿预查报告[R].2021.
The Third Geological Branch,Xinjiang Geological and Mineral Bureau.Preliminary Survey Report of South Waishixia Lithium Beryllium Deposit,Ruoqiang County,Xinjiang[R].2021.