研究论文

蛇绿岩中的花岗质岩石成因类型与构造意义

  • 李献华 ,
  • 李武显
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  • 中国科学院广州地球化学研究所,广东 广州 510640
李武显(1964-),男,湖北来凤县人,博士后,主要从事火成岩岩石学和岩石地球化学研究.E-mail:liwx@gig.ac.cn

收稿日期: 2002-07-15

  修回日期: 2002-10-25

  网络出版日期: 2003-06-01

基金资助

中国科学院知识创新工程重要方向项目“华南中生代盆地系统及动力学研究”(编号:KZCX2-102);国家自然科学基金重点项目“华南和华北地块对Rodinia全球超大陆事件的响应”(编号:40032010-B)资助.

ROCK TYPES AND TECTONIC SIGNIFICANCE OF THE GRANITOIDS ROCKS WITHIN OPHIOLITES

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  • Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China

Received date: 2002-07-15

  Revised date: 2002-10-25

  Online published: 2003-06-01

摘要

花岗质岩石在蛇绿岩的岩石组合中只占很小部分(通常<10%),但是对于蛇绿岩的成因研究,特别是对蛇绿岩形成和演化过程的精确年龄测定,具有重要的意义。简要回顾了蛇绿岩中花岗质岩石的研究历史。近年来的研究表明,蛇绿岩中的花岗质岩石不仅包括直接由大洋玄武质岩浆结晶分异形成的花岗质岩石,即传统意义上的大洋斜长花岗岩,还包括蛇绿岩在形成、演化过程中本身形成的和侵入的花岗质岩石。根据成因,可以将这些花岗质岩石分为 4类:结晶分异型花岗岩、剪切型花岗岩、俯冲型花岗岩和仰冲型花岗岩。系统地综述了它们的地球化学特征以及形成的构造背景。

本文引用格式

李献华 , 李武显 . 蛇绿岩中的花岗质岩石成因类型与构造意义[J]. 地球科学进展, 2003 , 18(3) : 392 -397 . DOI: 10.11867/j.issn.1001-8166.2003.03.0392

Abstract

The minor granitoids(general <10%) in the ophiolite are important for studying origin of the ophiolite, especially dating the precise ages of the ophiolites formation and evolution. It is simple review research history of the granitoids within the ophiolites in this paper. The recent research shows that granitoids rocks within the ophiolites include not only the granites formed by fractionation of MORB at low pressure, but also the granites which formed by partial melting of gabbros of ophiolites in shear zone or intruded it during the formation and evolution of the ophiolite. Based on the origin of the granitoids, they are subdivided into four types: fractionation-type;shearing-type;subduction-type, and obduction-type. The geochemical characteristics, tectonic setting and geological implication of the granitoids are systemically summarized in this paper. Discrimination and timing the different type granitoids within the ophiolites would precise constrained the times of the ophiolite evolution from spreading of ocean crust, subducting of ocean crust and obducting onto the continental crust. It is important for understanding the origin and evolution of the ophiolites.

参考文献

[1] Coleman R G, Peterman Z E. Oceanic plagiogranite[J]. Journal of Geophysical Research, 1975, 80: 1 099-1 108.

[2] Gilluly J. Keratophyres of eastern Oregon and the spilite problem[J]. American Journal of Science, 1935, 29: 171,225-252,336-352.

[3] Coleman R G, Donato M M. Oceanic plagiogranite revisited[A]. In: Barker F, ed. TrondhJemites, Dacites and Related Rocks[C]. Amsterdam: Elsevier, 1979. 149-168.

[4] Aumento F. Diorites from the mid-Atlantic ridge at 45°N[J]. Science, 1969, 165: 1 112-1 113.

[5] Aldiss D T. Plagiogranites from the ocean crust and ophiolites[J]. Nature, 1981, 289: 577-578.

[6] Dixon S, Rutherford M J. Plagiogranite as late-stage immiscible liquids in ophiolite and mid-ocean ridge suite: An experimental study[J]. Earth and Planetary Science Letters, 1979, 45: 45-60.

[7] Searle M P, Malpas J. The structure and metamorphism of rocks beneath the Semail ophiolite of Oman and their significance in ophiolite obduction[J]. Transactions of Royal Society, Edinburgh Earth Sciences, 1980, 71: 247-262.

[8] Searle M P, Malpas J. Petrochemistry and origin of sub-ophiolite metamorphic and related rocks in the Oman Mountains[J]. Journal of Geological Society of London, 1982, 139: 235-248.

[9] Spray J G, Williams G D. The sub-ophiolite metamorphic rocks of the Ballantrae igneous complex, SW Scotland[J]. Journal of Geological Society London, 1980, 137: 359-369.

[10] Pearce J A. High T/P metamorphism and granite genesis beneath ophiolite thrust sheets[J]. Ofioliti, 1989, 14: 195-211.

[11] Peters T, Kamber B S. Peraluminous, potassium-rich granitoids in the Semail Ophiolite[J]. Contribution to Mineralogy and Petrology, 1994, 118: 229-238.

[12] Pedersen R B, Malpas J. The origin of oceanic plagiogranites from the Karmoy ophiolite, western Norway[J]. Contribution to Mineralogy and Petrology, 1984, 88: 36-52.

[13] Flagler P A, Spray J G. Genration of plagiogranite by amphibolite anatexis in oceanic shear zones[J]. Geology, 1991, 19: 70-73.

[14] Sorenson S S, Grossman J N. Enrichment of trace elements in garnet amphibolites from a paleo-subduction zone: Catalina Schist, southern California[J]. Geochimica et Cosmochimica Acta , 1989, 53: 3 155-3 177.

[15] Sorensen S S. Petrology of amphibole-facies nafic and ultramafic rocks from Catalina schist, southern California: Metamorphism and magmatisation in a subduction zone metamorphic setting[J]. Journal of Metamorphical Geology, 1988, 6: 405-435.

[16] Bebout G E, Barton M D. Metamorphism during subduction: Products and possible paths in the Catalina schist, California[J]. Chemical Geology, 1993, 108: 61-92.

[17] Defant M J, Richerson P M, De Boer J Z, et al. Dacite genesis via both slab melting and differentiation: Petrogenesis of La Yeguada Vocanic Comlex, Panama[J]. Journal of Petrology, 1991, 32: 1 101-1 142.

[18] Martin H. Adakitic magmas: Modern analogues of Archean granitoids[J]. Lithospher, 1999, 46: 411-429.

[19] Key R W. Aleutian magnesian andesites: Melts from subducted Pacific Ocean crust[J]. Journal of Volcanology and Geothermal Research, 1978, 4: 117-132.

[20] Defant M J, Drummond M S. Derivation of some modern arc magmas by melting of subducted lithosphere[J]. Nature, 1990, 347: 662-665.

[21] Drummond M S, Defant M J. A model for trondhJemite-tonalite-dacite genesis and crustal growth via slab melting: Archean to modern comparisons[J]. Journal of Geophysical Research, 1990, 95: 21 503-21 521.

[22] Scarrow J H, Pease V, Fleutelot C, et al. The late Neoproterozoic Enganepe ophiolite, Polar Urals, Russia: An extension of the Cadomian arc?[J]. Precambrian Research, 2001, 110: 255-275.

[23] Li W X, Li X H. Adakite granites within the NE Jiangxi Ophiolites, South China: Geochemical and Nd isotopic evidence[J]. Precambrian Research, 2003,112:29-44.

[24] Amri I, Benoit M, Ceuleneer G. Tectonic setting for the genesis of oceanic plagiogranites: Evidence from a paleo-spreading structure in the Oman ophiolite[J]. Earth and Planetary Science Letters, 1996, 139: 177-194.

[25] Floyd P A, Yaliniz M K, Goncuoglu M C. Geochemistry and petrogenesis of intrusive and extrusive ophiolitic plagiogranites, Central Anatolian crystalline complex, Turkey[J]. Lithospher, 1998, 42: 225-241.

[26] Cox J, Searle M, Pedersen R. The petrogenesis of leucogranitic dykes intruding the northern Semail ophiolite, United Arab Emirates: Field relationships, grochemistry and Sr/Nd isotope systematics[J]. Contribution to Mineralogy and Petrology, 1999, 137: 267-287.

[27] Whitehead J, Dunning G R, Spray J G. U-Pb geochronology and origin of granitoid rocks in the Thetford Mines ophiolite, Canadian Appalachians[J]. Geological Society of American Bulletin, 2000, 112: 915-928.

[28] SkJerlie K P, Pedersen R B, Wennberg O P, et al. Volatile phase fluxed anatexis of sediments during late Caledonian ophiolite obduction: Evidence from the Sogneskollen granitic complex, west Norway[J]. Journal of Geological Society London, 2000, 157: 1 199-1 213.

[29] Pearce J A, Harris N B W, Tindle A G. Trace element discrimination diagrams for the tectonic interpretation of granitic rocks[J]. Journal of Petrology, 1984, 25: 956-983.

[30] Heltz R T. Phase relations of basalts in their melting range at PH2O = 5 kb as a function of oxygen fugacity: Part I. Mafic phase[J]. Journal of Petrology, 1973, 14: 249-302.

[31] Zhang Qi, Zhou Guoqing. Ophiolites of China[M]. Beijing: Science Press, 2001. 1-182.[张旗,周国庆. 中国蛇绿岩[M]. 北京:科学出版社,2001.1-182.]

[32] Li Xianhua, Zhou Guoqing, Zhao Jianxin, et al. SHRIMP ion probe zircon age of the NE Jiangxi ophiolite and its tectonic implications[J]. Geochimica, 1994, 23: 125-131. [李献华,周国庆,赵建新,. 赣东北蛇绿岩的离子探针锆石U-Pb年龄及其构造意义[J]. 地球化学,1994,232:125-131.]

[33] Jian Ping, Wang Xiaofeng, He Longqing, et al. U-Pb zircon dating of anothosite and plagiogranite from the JinshaJiang ophiolite belt[J]. Acta Petrologica Sinica, 1999, 15(4): 590-593. [简平,汪啸风,何龙清,. 金沙江蛇绿岩中斜长岩何斜长花岗岩的U-Pb年龄及地质意义[J]. 岩石学报,1999,15:590-593.]

[34] Jian Ping, Wang Xiaofeng, He Longqing, et al. U-Pb zircon dating of the Shuanggou ophiolite from Xinping county, Yunnan province[J]. Acta Petrologica Sinica, 1998, 14(2): 207-211. [简平,汪啸风,何龙清,. 云南新平县双沟蛇绿岩U-Pb年代学初步研究[J]. 岩石学报,1998, 14(2): 207-211.]

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