• 中国出版政府奖提名奖

    中国百强科技报刊

    湖北出版政府奖

    中国高校百佳科技期刊

    中国最美期刊

    Volume 25 Issue 1
    Jan.  2000
    Turn off MathJax
    Article Contents
    HAN Qing-jun, SHAO Ji-an, 2000. MINERAL CHEMISTRY AND METAMORPHIC p-t CONDITIONS OF GRANULITE XENOLITHS IN EARLY MESOZOIC DIORITE IN HARKIN REGION, EASTERN INNER MONGOLIA AUTONOMOUS REGION, CHINA. Earth Science, 25(1): 21-27.
    Citation: HAN Qing-jun, SHAO Ji-an, 2000. MINERAL CHEMISTRY AND METAMORPHIC p-t CONDITIONS OF GRANULITE XENOLITHS IN EARLY MESOZOIC DIORITE IN HARKIN REGION, EASTERN INNER MONGOLIA AUTONOMOUS REGION, CHINA. Earth Science, 25(1): 21-27.

    MINERAL CHEMISTRY AND METAMORPHIC p-t CONDITIONS OF GRANULITE XENOLITHS IN EARLY MESOZOIC DIORITE IN HARKIN REGION, EASTERN INNER MONGOLIA AUTONOMOUS REGION, CHINA

    • Received Date: 1999-06-15
    • Publish Date: 2000-01-25
    • The mafic granulite xenolith was first reported to have occurred in Early Mesozoic diorite in Harkin region, Eastern Inner Mongolia Autonomous Region, China. The preliminary research indicates that the basic granulite xenoliths are different from the Precambrian granulite exposed on the earth surface of the North China craton. The electron microprobe analysis was performed of the four main rock-forming minerals: orthopyroxene, clinopyroxene, biotite and plagioclase, in comparison with those of Precambrian granulite terrain. The major focus is on the research into the chemical composition of various major rock-forming minerals. In addition, the metamorphic p-t conditions for the granulite xenoliths are discussed. The research results show that the metamorphism of the xenoliths had reached the granulite facies at the metamorphic temperatures ranging from 850 ℃ to 900 ℃ and at the metamorphic pressures ranging from 0.6 GPa to 1.0 GPa. These mafic granulite xenoliths reflect the component features of the Early Mesozoic continental lower crust of the research region, providing some evidence for the reconstruction of the Early Mesozoic deep crustal structure.

       

    • loading
    • [1]
      邵济安, 韩庆军, 张履桥, 等. 内蒙古东部早中生代堆积杂岩捕虏体的发现[J]. 科学通报, 1999, 44(5) : 478~485. doi: 10.3321/j.issn:0023-074X.1999.05.004
      [2]
      张儒媛, 从柏林. 冀东迁西地区早太古代麻粒岩的矿物化学和结晶的P-T条件[J]. 中国科学, 1981, 7 : 855~868. http://www.cnki.com.cn/Article/CJFDTotal-JAXK198107008.htm
      [3]
      Deer W A, Howie R A, Zussman J. Rock-forming minerals. 2nd. Single-chain Silicates. Longman: Longman Group Limited, 1978.
      [4]
      Wood B J, Banno S. Garnet-orthopyroxene and or thopyroxene-clinopyroxene relationship in simple and complex systems. Cont Mineral Pe tro, 1973, 42: 109~124.
      [5]
      Wells R J. Py roxene thermometry in simple and complex systems[J]. Contr Mineral Petro, 1977, 62 : 129~139. doi: 10.1007/BF00372872
      [6]
      沈其韩, 徐惠芬, 张宗清, 等. 中国早前寒武纪麻粒岩[M]. 北京: 地质出版社, 1992.
      [7]
      贺高品, 卢良兆. 冀东和内蒙古东南部早前寒武纪变质作用演化[M]. 长春: 吉林大学出版社, 1991.
      [8]
      阎月华, 翟明国. 吉林桦甸太古代杂岩的矿物化学和变质作用温压条件[J]. 岩石学报, 1988, 3: 16~27. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB198803002.htm
      [9]
      靳是琴, 李殿超. 华北麻粒岩相岩石中的辉石[J]. 长春地质学院学报, 1986, 2: 30~36. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ198602002.htm
      [10]
      王时麒, 孙承志, 崔文元, 等. 内蒙古赤峰地区金矿地质[M]. 呼和浩特: 内蒙古人民出版社, 1994.150~159.
      [11]
      陈绍海, 张国辉, 周新华, 等. 汉诺坝玄武岩中麻粒岩类捕虏体的岩石学特征[J]. 岩石学报, 1998, 14(3) : 366 ~379. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB803.009.htm
      [12]
      李殿超. 冀东地区变质岩中斜方辉石的研究[J]. 岩石矿物学杂志, 1995, 14(2) : 185~190. https://www.cnki.com.cn/Article/CJFDTOTAL-YSKW502.010.htm
      [13]
      Boyd F R. A pyroxene geotherm[J]. Geochimet Cosmochim Acta, 1973, 37 : 2533~2546. doi: 10.1016/0016-7037(73)90263-9
      [14]
      Obata M. The solubility of Al2O3 in ortho pyroxenes in spinel and plagioclase peridotites and spinel pyroxenite [J]. Amer M iner, 1976, 61 : 804~816.
      [15]
      Dobretsov N L, Reverdatto V V, Sobolev V S, et al. Fatsiimetamorfizma[M]. Moscow : IzdNedra, 1970.
      [16]
      郑巧荣. 由电子探针分析值计算Fe3+和Fe2+[J]. 矿物学报, 1983, (1) : 55~62. doi: 10.3321/j.issn:1000-4734.1983.01.009
      [17]
      Bhattacharyya C. An evaluation of the chemical distinctions between igneous and metamorphicortho pyroxenes [J]. Amer Miner, 1971, 56 : 499~506.
      [18]
      Dobretsov N L, Sobolev V S, K hlestov V V. The facies of regional metamorphism at moderate pressures[M]. Translated by Brown D A. Canberra: Aust Natl Univ, Dep Geol Publ, 1973.
      [19]
      Wood B J. The solubility of alumina in orthopyroxene coexisting with garnet[J]. Contr Miner Petrol, 1974, 46: 1~15. doi: 10.1007/BF00377989
      [20]
      M acGregor I D, Basu A R. Geological problems in estimating mantle geothermal gradients[J]. Amer Miner, 1976, 61 : 715~724. doi: 10.1016/0040-1951(75)90067-0
      [21]
      V ejnar Z. Highly ferrous silicates from the Mutenin ferrodioritering intrusion, West Bohemia, Czeh[J]. Ustred Ustav Geol Vestn, 1975, 50(5) : 265~273.
      [22]
      阎月华. 几种镁铁矿物平衡共生的成分标志[J]. 地质科学, 1997, 32(3) : 267~274. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKX703.002.htm
      [23]
      [24]
      Rudnick R L, Tay lor S R. The composition and petrogenesis of the lower crust : axenolith study[J]. J Geophys Res, 1987, 92: 13981~14005. doi: 10.1029/JB092iB13p13981
      [25]
      Guitdo tti C V. Micas in metamorphic rocks[J]. Reviews in Mineralogy, 1984, 13 : 357~486.
      [26]
      张儒媛, 从柏林. 矿物温度计和矿物压力计[M]. 北京: 地质出版社, 1983.
      [27]
      叶慧文. 变质成因矿物研究的主要问题[J]. 长春地质学院学报, 1986, (1) : 107~117.
      [28]
      Rollinson H R. Garnet-pyroxene thermometry and barometry in the Scourie granulites, NW Scoland[J]. Lithos, 1981, 14 : 225~238. doi: 10.1016/0024-4937(81)90044-X
      [29]
      Green D H, Ringwood A E. An experimental investigation of the gabbro to eclogite transformation, its petrological applications[J]. Geochim et Cosmochim Acta, 1967, 31: 767~833. doi: 10.1016/S0016-7037(67)80031-0
      [30]
      Irving A J. Geochemical and high-pressure experimental studies of garnet pyroxenite and pyroxene granulite xenoliths from the Delegate basaltic pipes, Australia[J]. J Petrol, 1974, 15: 1~40.
      [31]
      Rushmer T. Experimental high-pressure granulites: some applications to natural maficx enoliths suites and Archean granulite terranes[J]. Geology, 1993, 21: 411~414. doi: 10.1130/0091-7613(1993)0212.3.CO;2
      [32]
      Halliday A N, Dickin A P. Formation and composition of the lower co ntinental crust : evidence from Scottish xenoliths suites. J Geophys Res, 1993, 98(B1) : 581~607.
    • 加载中

    Catalog

      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(5)  / Tables(2)

      Article views (4152) PDF downloads(16) Cited by()
      Proportional views

      /

      DownLoad:  Full-Size Img  PowerPoint
      Return
      Return