地球科学进展 ›› 1995, Vol. 10 ›› Issue (2): 148 -153. doi: 10.11867/j.issn.1001-8166.1995.02.0148

干旱气候变化与可持续发展 上一篇    下一篇

变质地质学新领域——超高压变质作用与地球动力学
刘晓春,曲玮   
  1. 中国科学院地球化学研究所  贵阳  550002
  • 收稿日期:1994-04-05 修回日期:1994-07-04 出版日期:1995-04-01
  • 通讯作者: 刘晓春
  • 基金资助:

    国家自然科学基金项目“中国中东部变质柯石英带的岩石学和矿物物理学及地质意义”(编号:49070099)资助.

FRONTIER OF METAMORPHIC GEOLOGY—ULTRAHIGH-PRESSURE METAMORPHISM AND GEODYNAMICS

Liu Xiaochun,Qu Wei   

  1. Institute of Geochemistry, Academia Sinica,Guiyang  550002
  • Received:1994-04-05 Revised:1994-07-04 Online:1995-04-01 Published:1995-04-01

简要总结了近年在欧亚大陆发现的超高压变质岩地质产状、岩石类型、结晶条件和构造位置等基本特征,对超高压变质作用及其地球动力学机制的研究现状及存在的问题进行了评述。基于对大别—苏鲁超高压变质带的研究成果,认为超高压变质作用可能是一种新型的区域变质作用,而目前所建立的任何一种地球动力学模型都不完善。建议今后在岩石学和矿物学研究基础上,加强对超高压变质杂岩的地球化学、构造地质学、实验岩石学及地球物理学等方面的研究。

The general features of ultrahigh-pressure metamorphic rocks discovered recently from Eurasian continent, including occurrence,rock type,crystalline condition and tectonic location,are summarized briefly and the progresses and problems of ultrahigh-pressure metamorphism and geodynamics are reviewed in this paper. According to the characteristics of protolith of eclogites,the discovery of the different types of non-mafic ultrahigh-pressure metamorphic rocks and the correlation of both P-T condition and age between retrograde metamorphism of eclogites and regional metamorphism of country rocks in the Dabie-Sulu district, ultrahigh-pressure metamorphism is considered to be a new type of regional metamorphism. The sequence of high-pressure metamorphic belt in the Dabie Mountains and the occurrence of coesite-bearing granulite retrograded from eclogite in eastern Shangdong suggest that the satisfactory geodynamic model for ultrahigh-pressure metamorphism has not been established up to now. On the basis of petrological and mineralogical works, the authors emphasize that geochemical,tectonic,experimental petrological and geophysical studies of ultrahigh-pressure metamorphic complex should be strengthened in the future.

[1] Smith D C. Coesite in the clinopyroxene in the Caledonides and its implication for geodynamics. Nature,1984,310:641-644.
[2] Schmadicke E. Quartz pseudomorphs after coesite in eclogues from the Saxoman Erzgebirge. Eur J Mineral,1991,3:231-238.
[3] Chesnokov B V and Popov V A. Increase in the volume of quartz grains in South Urals eclogite. Dokl Akad Nauk USSR ,1965 ,162:176-178.
[4] Becker H et al. Evidence from ultra-high-pressure marbles for recycling of sediment into the mantle. Nature,1992,358:745-748.
[5] Chopin C. Coesite and pure pyrope in high-grade blueschists of the western Alps,a first record and some consequences. Contrib Mineral Petrol, 1984,86:107-118.
[6] Reinecke T. Very-high-pressure metamorphism and uplift of coesite-bearing metasediments from the Zermatt-Saas Zone, Western Alps.Eur J Minera1,1991,3:7-17.
[7] Sobolev N V and Shatsky V S. Diamond inclusions in garnet from metamorphic rocks: a new environment for diamond formation. Nature,1990,343:742-745.
[8] Tagiri M and Bakirov A. Quartz pseudomorph after coesite in garnet form a garnet-chloritoid-talc schist, northern Tien-Shan,Kirghiz,USSR. Proc Japan Acad Sci,1990,66:135-139.
[9] Wang X, Liou J G and Mao H K. Coesite-bearing eclogue from the Dabie Mountains in central China. Geology, 1989,17;1085一1088.
[10] Wang Q. Ishiwatari A and Zhao Z et al. Coesite-bearing granulite retrograded from eclogite in Weihai, eastern China. Eur J Minera1,1993,5:141-152.
[11] Smith D C. A review of the peculiar mineralogy of the "Norwegian coesite-eclogite province", with crystal-chemical,petrological, geochemical and geodynamical model and an extensive bibliography. In: Smith D C(eds). Eclogites and Eclogite-facies Rocks. Amsterdam, Elsevier,1988. 1-206.
[12] Chopin C. Very-high-pressure metamorphism in the western Alps: implications for subduction crust. Philos Trans R Soc London, 1987,A321:183-197.
[13] 徐树桐,江来利,刘贻灿,张勇.大别山区(安徽部分)的构造格局和演化过程.地质学报,1992,(1):1-4.
[14] Schreeyer W. Subduction of continental crust to mantle depths:petrological evidence. Episodes,1988,11:97-104.
[15] Hsu K 1. Exhumation of high-pressure metamorphic rocks. Geology,1991,19:107-110.
[16] Dobretsov N L. Blueschists and eclogites: a possible plate tectonic mechanism for their emplacement from the upper mantle. Tectonophysics,1991,186:253-268.
[17] Aviged D. Exhumation of coesite-bearing rocks in the Dora hiaira massif(western Alps, Italy). Geology,1992,20:947-950.
[18] Okay A and Sengor C. Evidence for intracontinental thrust-related exhumation of the ultra-high-pressure rocks in China. Geology,1992,20:411-414.
[19] Cloos M. Flow mélanges:numerical modeling and geologic constraints on their origin in the Franciscan Subduction Complex, California. Geol Sci Am Bull,1982,93:330-345.
[20] Perchuk L L. Geodynamic models for origin of high/ultra-high pressure metamorphic complexes:a review. 29th IGC Abstract.1992. 2 of 3:596.

[1] 赵仁杰,鄢全树,张海桃,关义立,葛振敏,袁龙,闫施帅. 全球俯冲沉积物组分及其地质意义[J]. 地球科学进展, 2020, 35(8): 789-803.
[2] 李大鹏,陈岳龙,靳野. 板块俯冲带研究中的数值实验[J]. 地球科学进展, 2010, 25(6): 582-596.
[3] 史斗,刘文汇,郑军卫. 深层气理论分析和深层气潜势研究[J]. 地球科学进展, 2003, 18(2): 236-244.
[4] 赵振华,刘秉光,李朝阳. 我国与寻找超大型矿床有关的基础研究进展[J]. 地球科学进展, 2001, 16(2): 184-188.
[5] 王强,许继锋,赵振华. 一种新的火成岩——埃达克岩的研究综述[J]. 地球科学进展, 2001, 16(2): 201-208.
[6] 陈增强,胡瑞华,刘立嵩. 中国地壳运动观测网络在地球科学研究中的应用前景[J]. 地球科学进展, 2000, 15(4): 421-425.
[7] 朱介寿. 下地幔及核幔边界结构及地球动力学[J]. 地球科学进展, 2000, 15(2): 139-142.
[8] 孙和平,许厚泽,徐建桥,柳林涛. 重力场的潮汐变化观测及其研究[J]. 地球科学进展, 2000, 15(1): 53-57.
[9] 倪志耀,王仁民,袁建平.

元古宙蛇绿岩研究中有关问题的讨论[J]. 地球科学进展, 1999, 14(5): 468-474.

[10] 许厚泽,孙和平. 我国重力固体潮实验研究进展[J]. 地球科学进展, 1998, 13(5): 415-422.
[11] 郑永飞,李曙光,陈江峰. 化学地球动力学[J]. 地球科学进展, 1998, 13(2): 121-128.
[12] 周鼎武,张成立,刘颖宇. 大陆造山带基底岩块中的基性岩墙群研究——以南秦岭武当地块为例[J]. 地球科学进展, 1998, 13(2): 151-156.
[13] 王军芝,聂高众. 90年代国际岩石圈计划研究进展[J]. 地球科学进展, 1998, 13(1): 27-33.
[14] 李院生,卢焕章,陈晓枫,李兆麟. 流体作用在地球动力学演化过程中的意义[J]. 地球科学进展, 1997, 12(2): 138-143.
[15] 孙和平,许厚泽. 国际地球动力学合作项目的实施与展望[J]. 地球科学进展, 1997, 12(2): 152-157.
阅读次数
全文


摘要