2022 Vol. 41, No. 9
Article Contents

CAI Yunhua, TAN Hua, ZHU Huipai, XU Bolun, XIONG Bin, WU Shengbo. Characteristics and attribution of basic volcanic rocks in Liyuan-Labai township area, Yunnan Province[J]. Geological Bulletin of China, 2022, 41(9): 1624-1633. doi: 10.12097/j.issn.1671-2552.2022.09.011
Citation: CAI Yunhua, TAN Hua, ZHU Huipai, XU Bolun, XIONG Bin, WU Shengbo. Characteristics and attribution of basic volcanic rocks in Liyuan-Labai township area, Yunnan Province[J]. Geological Bulletin of China, 2022, 41(9): 1624-1633. doi: 10.12097/j.issn.1671-2552.2022.09.011

Characteristics and attribution of basic volcanic rocks in Liyuan-Labai township area, Yunnan Province

  • There are basic volcanic rocks with banded distribution in the Zhuazi-Liyuan-Labai township area of Northwest Yunnan Province.Previous views concerning the attribution of basic volcanic rocks are controversial.According to the investigation and research, the basic volcanic rocks are distributed in the westernmost margin of the Yangtze Block, mainly composed of olivine basalt, pyroxene basalt, volcanic breccia, et. The rocks have pillow structure and columnar joint, showing the eruption environment of water land interaction; the petrological geochemistry shows enriched alkali, low potassium, high titanium, enriched LREE, enriched LILE and enriched HFSE characteristics; the basic volcanic rocks in this area are generally similar to the Permian Emeishan basalt in Lijiang-Binchuan area of northwest Yunnan Province, and belong to the Emeishan basalt formation in Lijiang stratigraphic regionalization.In addition, a number of biological fossils were obtained from the bioclastic limestone intercalations in the middle and lower part of the basic volcanic rocks.The age is identified as Early—Middle Permian, which shows that the basic volcanic rocks were formed in the Early—Middle Permian.

  • 加载中
  • [1] 潘桂棠, 王立全, 张万平, 等. 青藏高原及邻区大地构造图及说明书(1: 1500000)[M]. 北京: 地质出版社, 2013.

    Google Scholar

    [2] 王立全, 潘桂棠, 丁俊, 等. 青藏高原及邻区地质图及说明书(1: 1500000)[M]. 北京: 地质出版社, 2013.

    Google Scholar

    [3] 潘桂棠, 李兴振, 王立全, 等. 青藏高原及邻区大地构造单元初步划分[J]. 地质通报, 2002, 21(11): 701-707.

    Google Scholar

    [4] 王保弟, 王立全, 王冬兵, 等. 三江昌宁-孟连带原-古特提斯构造演化[J]. 地球科学, 2018, 43(8): 2527-2550.

    Google Scholar

    [5] Middlemost E A K. Naming materials in the magma/igneous rock system[J]. Earth Science Reviews, 1994, 37(3/4): 215-224.

    Google Scholar

    [6] 徐义刚, 钟孙霖. 峨眉山大火成岩省: 地幔柱活动的证据及其熔融条件[J]. 地球化学, 2001, 30(1): 1-9.

    Google Scholar

    [7] 吕劲松, 肖渊甫, 邓江红, 等. 滇西北峨眉山玄武岩与冈达概组下段玄武岩对比研究[J]. 岩石矿物学杂志, 2013, 32(1): 73-89.

    Google Scholar

    [8] 倪平泽, 肖龙, 何琦, 等. 滇西丽江树底桥及宁蒗万马场二叠纪玄武岩地球化学特征及成因[J]. 矿物岩石, 2007, 27(1): 107-116.

    Google Scholar

    [9] Sun S S, Mcdonough W F. Chemical and isotopic systematics of oceanic basalt: implications for mantle composition and processes[J]. Geological Society of London Special Publication, 1989, 42(1): 313-345.

    Google Scholar

    [10] 汪云亮, Hughes S S, 童纯菡, 等. 峨眉山玄武岩地球化学和大陆地幔演化[J]. 成都地质学院学报, 1987, 14(3): 62-77.

    Google Scholar

    [11] 张招崇, 王福生, 郝艳丽, 等. 峨眉山大火成岩省中苦橄岩与其共生岩石的地球化学特征及其对源区的约束[J]. 地质学报, 2004, 78(2): 171-180.

    Google Scholar

    [12] 汪云峰, 张招崇, 王丽娟, 等. 峨眉山大火成岩省虎跳峡和金安二叠纪玄武岩的地球化学特征及其对源区的约束[J]. 岩石学报, 2013, 29(12): 4387-4403.

    Google Scholar

    [13] 汪云亮, 张成江, 修淑芝. 玄武岩类形成的大地构造环境的Th/Hf-Ta/Hf图解判别[J]. 岩石学报, 2001, 17(3): 413-421.

    Google Scholar

    [14] Lassiter J C, DePaolo D J. Plume/Lithosphere Interaction in the Generation of Continental and Oceanic Flood Basalts: Chemical and Isotopic Constraints[C]//Large Igneous Provinces: Continental, Oceanic, and Planetary Flood Volcanism. Washington DC: American Geophysical Union(AGU), 2013.

    Google Scholar

    [15] 张招崇, Mahoney J, 王福生, 等. 峨眉山大火成岩省西部苦橄岩及其共生玄武岩的地球化学: 地幔柱头部熔融的证据[J]. 岩石学报, 2006, 22(6): 1538-1552.

    Google Scholar

    [16] 朱士飞, 秦勇, 钱壮志, 等. 云南省丽江—宾川地区二叠纪玄武岩地球化学特征及其构造背景研究[J]. 矿物岩石, 2008, 28(1): 64-71.

    Google Scholar

    [17] 姜常义, 钱壮志, 姜寒冰, 等. 云南宾川—永胜—丽江地区低钛玄武岩和苦橄岩的岩石成因与源区性质[J]. 岩石学报, 2007, 23(4): 777-792.

    Google Scholar

    [18] Dan M, O'Nions R K. Partial Melt Distributions from Inversion of Rare Earth Element Concentrations[J]. Journal of Petrology, 1991, 32(5): 1021-1091.

    Google Scholar

    [19] 张雪, 翁凯, 赵晓健, 等. 新疆东天山卡拉塔格二叠纪火山岩成因及构造意义[J]. 吉林大学学报(地球科学版), 2021, 51(4): 1119-1138.

    Google Scholar

    [20] Wang K, Plank T, Walker J D, et al. A mantle melting profile across the Basin and Range, SW USA[J]. Journal of Geophysical Research: Solid Earth, 2002, 107(B1): ECV 5-1-ECV 5-21.

    Google Scholar

    [21] Lassiter J C, Depado D J. Plume/lithosphere interaction in the generation of continental and oceanic flood basalts: Chemical and isotopic constraints[M]. Washington D C. American Geophysical Union Geophysical Monograph Series, 1997: 335-355.

    Google Scholar

    [22] Pearce J A, Norry M J. Petrogenetic implications of Ti, Zr, Y, and Nb variations in volcanic rocks[J]. Contributions to Mineralogy & Petrology, 1979, 69(1): 33-47.

    Google Scholar

    [23] Bao J F, Zhao Y J, Sun Z B, et al. Characteristics and tectonic environment of the Late Triassic volcanic rocks in the Baoshan Block of western Yunnan[J]. Advances in Geosciences, 2020, 10(5): 385-403.

    Google Scholar

    [24] Meschede M, 韩宝福. 一种用Nb-Zr-Y图解判别各种洋中脊玄武岩和大陆拉斑玄武岩类型的方法[J]. 地质地球化学, 1988, (12): 31-34.

    Google Scholar

    云南省地质局. 1: 20万永宁幅区域地质调查报告. 1980.

    Google Scholar

    云南省地质矿产局区域地质矿产调查大队. 1: 25万中甸县幅、贡山县幅区域地质调查报告. 2003.

    Google Scholar

  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Figures(7)

Tables(3)

Article Metrics

Article views(1436) PDF downloads(96) Cited by(0)

Access History

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint