全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...

板块构造学说面临的挑战

, PP. 265-274

Keywords: 板块构造学说,大火成岩省,大陆增长,壳幔耦合

Full-Text   Cite this paper   Add to My Lib

Abstract:

板块构造学说揭示了海底扩张和板块的水平运动现象,阐明了与板块边界相联系的岩浆活动。但大量资料表明地球历史上岩石圈板块与软流圈是同步耦合运动的,而不是在软流圈上滑移。全球扩张与俯冲的不对称性现象也是不吻合于板块构造理论所期望的。安第斯弧作为洋陆俯冲的典范在地球物理和地球化学上均缺少证据。对于与俯冲带相关的弧后引张、大陆增生、地壳物质返回地幔和成矿作用方面均存在较多的问题。大火成岩省所揭示的岩浆活动现象超越了板块构造的格局,并发生在整个地质历史时期和更广泛的地域范围。大火成岩省学说所解释的大陆增长、地壳物质返回地幔和成矿作用过程完全不同于板块构造学说。驱动地幔柱的深地幔对流假说允许岩石圈板块与下伏软流圈一起运动,吻合铅同位素所揭示的岩石圈与软流圈长期耦合的规律。

References

[1]  Zhu B Q, Hu Y G, Chang X Y, Xie J and Zhang Z W. 2005. The Emeishan large igneous province originated from magmatism of a primitive mantle plus subducted slab. Russian Geol Geophys, 46(9): 904-921.
[2]  Zhu B Q, Hu Y G, Zhang Z W and Chang X Y. 2003. Discovery of the copper deposits with features of the Keweenawan type in the border area of Yunnan?Guizhou Provinces. Science in China (D), 46(supp): 60-72.
[3]  Zhu B Q, Wang H F, Chen Y W et al. 2004. Geochronological and geochemical constraint on the Cenozoic extension of Cathaysian lithosphere and tectonic evolution of the border sea basins in East Asia. J Asian Earth Sci, 24: 163-175.
[4]  Zou R, Zhu B Q, Sun D Z and Chang X Y. 1997. Geochronological study on crustal?mantle evolution and mineralization in the Red River zone. Geochimica, 26(2): 46-56 (in Chinese with English abstract).
[5]  邹日, 朱炳泉, 孙大中, 常向阳. 1997. 红河成矿带壳幔演化与成矿作用的地质年代学研究. 地球化学, 26(2): 46-56.
[6]  Barley M E, Pickard A L and Sylvester P J. 1997. Emplacement of a large igneous province as a possible cause of banded iron formation 2.45 billion years. Nature, 385: 55-58.
[7]  Chen Guoda, Peng Shenglin and Dai Tagen. 2005. Historistic?dynamic tectonic differentiation of E?W of central Asia continental crustobody and its significance. Geotectonica et Metallogenia, 29(1):7-16 (in Chinese with English abstract).
[8]  Chiaradia M and Fontbote L. 2002. Lead isotopic systematics of Late Cretaceous?Tertiary Andean arc magmas and associated ores between 8°N and 40°S: evidence for latitudinal mantle heterogeneity beneath the Andes. Terra Nova, 14: 337-342.
[9]  Ernst R E, Buchan K L and Compbell I H. 2005. Frontier in large igneous province research. Lithos, 79:271-297.
[10]  Frey F A, Coffin M F, Wallace P J et al. 2000. Origin and evolution of a submarine large igneous province: the Kerguelen Plateau and Broken Ridge, southern Indian Ocean. Earth Planet Sci Lett, 28: 73-89.
[11]  Gerasimenko M D and Kato T. 2000. Establishment of the three?dimensional reference frame by space geodetic measurements. Earth Planets Space, 52: 959-963.
[12]  Gorbatov B L and Kennett N. 2003. Joint bulk?sound and shear tomography for Western Pacific subduction zones. Earth Planet Sci Lett, 210: 527-543.
[13]  Gutscher M A, Maury R C. Eissen J P et al. 2000. Can slab melting be caused by flat subduction? Geology, 28: 535-538.
[14]  Hawkins J W, Lonsdale P F, Macdougall J D and Volpe A M. 1990. Petrology of the axial ridge of the Marianna Trough backarc spreading center. Earth Planet Sci Lett, 100: 226-250.
[15]  Hickey?Vargas R. 1998. Origin of the Indian Ocean type isotopic signature in basalts from Philippine Sea plate spreading centers: An assessment of local versus large?scale processes. J Geophy Res, 103 (B9): 20963-20979.
[16]  Huang Z L, Cheng J and Han R S. 2004. Geochemistry and ore?formation of the Huize super?large lead?zinc deposit, Yunnan province, China: Discussion on the relationship between Emeishan flood basalts and lead?zinc mineralization. Beijing: Geological Press (in Chinese).
[17]  Johnson K E, Harmon S, Richardson M et al. 1996. Isotope and trace element geochemistry of Augustine volcano, Alaska: Implications for magmatic evolution. J Petrol, 37: 95-115.
[18]  Kraemer B. 1999.A geochemical traverse across the Middle Miocene magmatic arc in the southern part of the central volcanic zone of the Andes (ZVZ, 25°~26°S, 67°~69°W). Berliner: Geowiss ABH.
[19]  Kusky T M and Li J?H. 2003. Paleoproterozoic tectonic evolution of the North China Craton. J Asian Earth Sci, 22: 383-397.
[20]  Lassiter J C, Blichert?Toft J, Hauri E H at al. 2003. Isotope and trace element variations in lava from Raivavae and Rapa, Cook?Austral islands: Constraint on the nature of HIMU and EM?mantle and the origin of mid?plate volcanism in French Polynesia. Chem Geol, 202:115-138.
[21]  Lucassen F, Escayola M, Romer R L et al. 2002. Isotopic composition of Late Mesozoic basic and ultrabasic rocks from the Andes 23°S~32°S?Implications for the Andean mantle. Contrib Mineral Petrol, 143: 336-349.
[22]  Lustrino M. 2005. How the delamination and detachment of lower crust can influence basaltic magmatism. Earth Sci Rev , 72: 21-38.
[23]  Mahoney J J, Frei R, Tejada M L G., Mo X X, Leat P T and Nagler T F. 1998. Tracing the Indian Ocean mantle domain through time: Isotopic results from old west Indian, East Tethyan, and South Pacific seafloor. J Petrol, 39: 1285-1306.
[24]  Mamani M, W?rner G, Hartmann G et al. 2005. A GIS?based isotopic map of the central Andes (13°S~28°S) and implications for ore formation. 6th International Symposium on Andean. Geodynamics(Barcelona), extended Abstract: 464-467.
[25]  Mann P and Taira A. 2004. Global tectonic significance of the Solomon Islands and Ontong Java Plateau convergent zone. Tectonophysics, 389:137-190.
[26]  Naldrett A J, Lightfoot P C, Fedorenko V, Doherty W and Gorbachev N S. 1992. Geology and geochemistry of intrusions and flood basalt of the Noril’sk region, USSR, with implications for the origin of the Ni?Cu ores. Ecol Geol, 87: 975-1004.
[27]  Ojakangas R W, Morey G B and Green J C. 2001. The Mesoproterozoic midcontinent rift system, Lake Superior region, USA. Sedimentary Geology, 141-142: 421-442.
[28]  Pirajno F. 2000. Ore deposits and mantle plumes. Dordrecht: Kluwer Academic Publishers.
[29]  Pubellier M, Monnier C, Maury R et al. 2004. Plate kinematics, origin and tectonic emplacement of supra?subduction ophiolites in SE Asia. Tectonophysics, 392: 9-36.
[30]  Pyle D G, Christie D M and Mahoney J J. 1992. Resolving an isotopic boundary with in the Australian Antarctic discordance. Earth Planet Sci Lett, 112: 161-178.
[31]  Robaudo S and Harrison C. 1993. Plate tectonics measured from SLR and VLBI global data. In: Smith D and Turcotte D (eds). Contributions of space geodesy to geodynamics: Crustal dynamics. 51-72, AGU, Washington D C.
[32]  Sharma M. 1997. Siberian traps. In: Mahoney J J and Coffin M F (eds). Large igneous provinces: Continental, oceanic, and planetary flood volcanism. American Geophysical Union Geophysical Monograph, 100: 273-295.
[33]  Spicak A, Hanus V and Vanek J. 2004. Seismicity pattern: an indicator of source region of volcanism at convergent plate margins. Physics of The Earth and Planetary Interiors, 141: 303-326.
[34]  Tardy M, Lapierre H, Struik L C et al. 2001. The influence of mantle plume in the genesis of the Cache Creek oceanic igneous rocks: implications for the geodynamic evolution of the inner accreted terranes of the Canadian Cordillera. Can J Earth Sci, 38: 515-534.
[35]  The ANCORP working group. 1999. Seismic reflection image revealing offset of Andean subduction?zone earthquake locations into oceanic mantle. Nature, 397: 341-344.
[36]  Thompson P M E, Kempton P D, White R V et al. 2004. Hf?Nd isotope constraints on the origin of the Cretaceous Caribbean plateau and its relationship to the Galápagos plume. Earth Planet Sci Lett, 217: 59-75.
[37]  Tomlinson K Y and Condie K C. 2001. Archean mantle plumes: evidence from greenstone belt geochemistry. In: Ernst R E and Buchan K L (eds). Mantle plumes: Their identification through time, special paper. Geological Society of America, 352: 341-357.
[38]  Wingate M T D, Pirajno F and Morri P A. 2004. Warakurna large igneous province: A new Mesoproterozoic large igneous province in west?central Australia. Geology, 32:105-108.
[39]  Xu J and Han Y. 1996. High radiogenic Pb?isotope composition of ancient MORB?type rocks from Qinling area?Evidence for the presence of Tethyan?type oceanic mantle. Science in China (D), 39(Supp): 33-42.
[40]  Zhang B L. 1994. Geochemical study of the lithosphere, tectonism and metallogenesis in the Qinling?Dabashan region. Wuhan: Press of China University of Geosciences (in Chinese).
[41]  Zhang B L, Zhang H F, Zhao Z D and Ling W L. 1996. Geochemical subdivision and evolution of the lithosphere in East Qinling and adjacent regions?implications for tectonics. Science in China (D), 39(3): 245-255.
[42]  Zhang G W, Meng Q G and Yu Z P. 1996. Orogenesis and dynamics of the Qingling Orogen. Science in China (D), 39:225-234.
[43]  Zhang L G. 1995. Block?geology of eastern Asia lithosphere. Beijing: Science Press (in Chinese).
[44]  Zhang S Q, Mahoney J J, Mo X X, Ghazi A M, Milani L, Crawford A J, Guo T Y and Zhao Z D. 2005. Evidence for a widespread Tethyan upper mantle with Indian?Ocean?type isotopic characteristics. J Petrol, 21: 1-30.
[45]  Zhang Z C, Guo Z J and Liu S W. 1996. The geochemical characteristics and tectonic significance of the mafic dyke swarm in the Kurktag, Xingjiang. In: Collected Works of International Symposium on Geological Sciences. Beijing: Seismological Press, 124-131.
[46]  Zhou M F, Robinson P T, Lesher C M, Keays R R, Zhang C-J and Malpas J. 2005. Geochemistry, petrogenesis and metallogenesis of the Panzhihua gabbroic layered intrusion and associated Fe?Ti?V oxide deposits, Sichuan Province, SW China. J Petrol, 46(11): 2253-2280.
[47]  Zhu B Q. 2001. Geochemical provinces and geochemical steep zones. Beijing: Science Press (in Chinese).
[48]  陈国达.2005.自主创新研究亚洲陆海大地构造与成矿学之必要.大地构造与成矿学,29(1):5-6.
[49]  陈国达,彭省临,戴塔根.2005.亚洲大陆中部壳体东、西部历史-动力学的构造分异及其意义. 大地构造与成矿学,29(1): 7-16.
[50]  黄智龙, 陈进, 韩润生. 2004. 云南会泽超大型铅锌矿地球化学及成因――兼论峨眉山玄武岩与铅锌矿的关系. 北京:地质出版社.
[51]  张本仁. 1994. 秦巴岩石圈构造及成矿规律地球化学研究. 武汉: 中国地质大学出版社.
[52]  张理刚. 1995. 东亚岩石圈地体地质. 北京:科学出版社.
[53]  朱炳泉. 2001. 地球化学省与地球化学急变带. 北京:科学出版社.
[54]  Ben?Avraham Z, Nur A, Jones D et al. 1981. Continental accretion: from oceanic plateau to allochthonous terranes. Science, 213, 47-54.
[55]  Bogdanov N and Dobretsov N. 2002. The Okhotsk volcanic oceanic plateau. Russian Geology and Geophysics, 43: 87-99.
[56]  Borg L E, Clynne M A and Mcmillan N J. 1997. The variable role of slab?derived fluids in the generation of a suite of primitive calc?alkaline lavas from the southernmost Cascade, California. Can Mineral, 35: 425-452.
[57]  Cannon W F and Suzanne W N. 1999. Geology and mineral deposits of the Keweenaw Peninsula, Michigan. U S Geological Survey Open?File Report, 99-149.
[58]  Chen Guoda. 2005. On the necessity of initiating geotectonics and metallogeny study in Asian land and sea areas. Geotectonica et Metallogenia, 29(1): 5-6 (in Chinese with English abstract).
[59]  Chung S L and Jahn B M. 1995. Plume?lithosphere interaction in generation of the Emeishan flood basalts at the Permian?Triassic boundary. Geology, 23: 889-892.
[60]  Conrey R M, Hooper P R, Larson P B et al. 2001. Trace element and isotopic evidence for two types of crustal melting beneath a high Cascade volcanic center. Contrib Mineral Petrol, 141: 710-732.
[61]  Dobretsov N L. 2005. 250 Ma large igneous provinces of Asia: Siberian and Emeishan traps (plateau basalts) and associated granitoids. Russian Geol Geophys, 46(9): 847-868.
[62]  Dostal J, Cousens B and Dupuy C. 1998. The incompatible element characteristics of an ancient subducted sedimentary component in ocean island basalts from French Polynesia. J Petrol, 39:937-952.
[63]  Ernst R E and Buchan K L. 2003. Recognizing mantle plume in the geological record. Ann Rev Earth Planet Sci, 31: 469-523.
[64]  Garzanti E, Le Fort P and Sciunnach D. 1999. First report of Lower Permian basalts in South Tibet: Tholeiitic magmatism during break?up and incipient opening of Neotethys. J Asian Earth Sci, 17: 533-546.
[65]  George R M, Turner S P and Hawkesworth C J. 2003. Melting processes and fluid and sediment transport rates along the Alaska?Aleutian arc from an integrated U?Th?Ra?Ba isotope study. J Geophys Res, B108 (5): ECV 6?1?ECV 6?25.
[66]  Romas V A. 1999. Plate tectonic setting of the Andean Cordillera. Episodes, 22: 183-190.
[67]  Schissel D and Smail R. 2001. Deep?mantle plumes and ore deposits. In: Ernst R E and Buchan K L (eds). Mantle plume: Their identification through time. GSA Am Spec Pap, 352: 291-322.
[68]  Schott B and Schmel H. 1998. Delamination and detachment of a lithospheric root. Tectonophysics, 296: 225-247.
[69]  Schubert G and Sandwell D. 1989. Crustal volumes of the continents and of oceanic and continental submarine plateaus. Earth Planet Sci Lett, 92: 234-246.
[70]  Sengor A M. 1993. Evolution of the Altaid tectonic collage and Paleozoic crustal growth in Eurasia. Nature, 364: 298-306.

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133