东天山平顶山巨眼球状片麻状花岗岩特征及成因
Characteristics and genesis of the Pingdingshan megaaugen gnelssic granite in the eastern Tianshan Mountain areas
-
摘要: 摘要本文以东天山平顶山岩体为例,探讨中天山晋宁旋回晚期巨眼球状片麻状花岗岩的特征及其形成机制。野外地质关系、岩相学、岩石化学、稀土元素、微量元素和同位素研究表明,平顶山岩体是岛弧钙碱性火山-沉积岩系经原地改造的产物,其Rb—Sr等时线年龄为927Ma.花岗岩形成作用的动力、热力来源可能与碰撞后天山岩石圈的拆沉有关。拆沉导致的底侵和内侵引发了地壳岩石的韧性剪切,剪切后的岩石有利于部分熔融、熔体-流体运移和化学反应,而熔体和流体的作用反过来又会促进韧性剪切,并将较浅层次的变形变质岩石改造为片麻状花岗岩。平顶山岩体的成岩作用体现了部分熔融、韧性剪切和流体作用的相互反馈,也是这些作用的共同产物。这种原地片麻状花岗岩的成岩过程主要为深源熔体和流体与原岩的相互作用,并使原岩发生不同程度的部分熔融,因而其地球化学特征同时受到原岩和外来熔体-流体的控制。底侵和内侵是造山过程晚期-期后挤压-拉张转折期地壳垂向增生的重要方式,而平顶山这类片麻状花岗岩则是这种垂向增生的产物。Abstract: Taking the Pingdingshan granite as an example, this paper investigates characteristics and genesis of augen gneissic granites of the late Jinning Cycle in the eastern Tianshan Mountain areas. Field relations, petrography, petrochemistry, rare earth elements, trace elements and isotopes indicate that the Pingdingshan granite, with a Rb-Sr isochron age of 927 Ma, was formed essentially by in situ transformation of metamorphosed island arc calc-alkaline volcanosedimentary rocks. Driving factors including heat could be ascribed to post-collisional delamination of the Tianshan lithosphere. Delamination-induced underplating and intraplating caused ductile shearing of the overlying crustal rock, such that partial melting, melt and fluid migration, and chemical reactions were highly enhanced, whereas melts and fluids themselves promoted further ductile shearing and transformed the deformed and metamorphosed rocks at higher levels into the gneissic granite. Formation of the this granite is resultant from a complex feed back of partial melting, ductile shearing and fluid activity. Petrogenesis being dominated by interaction of deep-sourced melts and fluids with protoliths in accompany with minor partial melting, geochemistry of such a kind of in situ gneissic granites is constrained by both protoliths and external melts and fluids. Underplating and intraplating are important manners of vertical accretion of the crust during late- to post-orogenic compresion-exention conversion, and gneissic granites like that at Pingdingshan are produced just by such a type of vertical accretion.
-
Key words:
- Augen granite /
- Underplating /
- Intraplating /
- Ductile shear zone /
- Pingdingshan /
- Tianshan Mountains /
- Xinjiang
-
[1] Allègre CJ, and 35 others. 1984. Structure and evolution of the Himalaya-Tibet orogenic belt. Nature, 307:17 - 22
[2] Barboza SA, Bergantz GW, Brown M. 1999. Regional gTanulite faciesmetamorphism in the lvrea zone: Is the Mafic Complex the smokinggun or a red herring? Geology, 27:447 -450
[3] Bell TH. 1985. Deformation partitioning and porphyroblast rotation in metamorphic rocks: a radical reinterpretation. J. Meta. Geol. , 3:109 - 118
[4] Bell TH, Johnson SE. 1989. The role of deformation partitioning in the deformation and recrystallization of plagioclase and K-feldspar in the Woodroffe thrust mylonite zone, central Australia. J. Meta. Geol. ,7:151 -168
[5] Best MG. 1982. Igneous and Metamorphic petrology. W. H. Freeman and Company, NewYork, 1 - 63
[6] Bickle MJ, Hawkesworth CJ, England PC, Athey D. 1975. A preliminary thermal model for regional metamorphism in the Eastern Alps. Earth Planet Sci. Lett. , 26:13 -28
[7] Boulter CA. 1987. The golden Mile, Kalgoorlie: A giant gold deposit localized in ductile shear zone by structurally induced infiltration ofan auriferous metamorphic fluid, Econ. Geol. , 82:1661 -1678
[8] Boynton WV. 1984. Geochemistry of the rare earth elements: meteorite studies. In: Henderson P. ( ed. ), Rare earth element geochemistry. Elservier, 63 - 114
[9] Brown M. 1994. The generation, segregation, ascent and emplacement of granitic magma: the migmatite to crustally-derived granite connection in thickened orogens. Earth-Sciences Reviews. 36( 1 ): 83 -132
[10] Brown M, Solar GS. 1999. The mechanism of ascent and emplacement of granite magma during transpress-ion: a syntectonic granite paradigm.Tectonophisics, 312: 1 - 33F
[11] Burg JP, Chen GM. 1984. Tectonics and structural zonation of southern Tibet, China. Nature, 311:219-223
[12] Burrett CF. 1972. Plate tectonics and the Hercynian orogen. Nature,239:155 - 157
[13] Castro A, Corretg LG, El-Biad C, El-Hmidi H, Fern ndez C, Patio D.2000. Experimental constraints on Hercynian anatexis in the Iberian Massif, Spain. J. Petrol. , 41:1471 -1488
[14] Chappell BW. 1999. Aluminium saturation in I-and S-type granites and the characterization of fractionated haplogranites. Lithos, 46:535 -551
[15] Chappell BW, White A J R. 1974. Two contrasting granite types.Pacific. Geol. , 8:173 - 174
[16] Chappell BW, White AJR. 1992. I-and S-type granites in the Lachan Fold Belt. Trans. Royal. Soc. Edinburgh. 83:1- 26. Also Geol.Soc. Amer. Spec. Paper, 272:1 - 26
[17] Chen YJ. 1996. Fludization model for intracontinental collision and its metallogenic significance: theoretical inference and evidences from gold deposits, the eastern Qinling Mountains. Earth Science Frontiers, 3(3 -4) :282 -289 ( in Chinese)
[18] Chen YJ, Sui YH, Pirajno F. 2003. Exclusive evidence for CMF model and a case of orogenic silver deposits: Isotope geochemistry of the Tieluping silver deposit, east Qinling orogen. Acta Petrologica Siica,19(3): 551 -568 (in Chinese)
[19] Chen YL, Wang Z G. 1993. Geochemistry of granites from eastern Tianshan Mountains, Xinjiang. Geochemistry, 3: 288- 302 (in Chinese)
[20] Chen YL. 1999. Geochemistry of granitoids from the Eastern Tianshan and the Northern Qinling belt. Beijing: Geological Publishing House, 1 - 141 (in Chinese)
[21] Clarke DB. , 1992, Granitoid Rocks. Chapman & Hall. London. 1 -283
[22] Clemens JD. 2003. S-type granitic magmas-petrogenetic issues, models and evidence. Earth-Science Reviews, 61:1 -18
[23] Collerson KD. 1976. Composition and structural state of alkali feldspar from high-grade metamorphic rocks, central Australia. 61:200 - 211
[24] Collins W J. 1998. Evaluation of petrogenetic models for Lachlan Fold Belt granitoids: implications for crustal architecture and tectonic models. Austrian Journal of Earth Sciences, 45:483 -500
[25] Cullers RL, Graf JL. 1984. Rare Earth elements in igneous rocks of the continental crust: intermediate and silicic rocks. In: Henderson, P.(ed), Rare Earth Element Geochemistry. Amsterdam: Elsevier Science: 275-316
[26] Davis JH, Blanckenburg F. 1995. Slab breakoff:: A model of lithosphere detachment and its test in the magmatism and deformationof collisional orogens, Earth: Planet. Sci. Lett. , 129: 85 - 102
[27] Davis JH, Stevenson DJ. 1992. Physical model of source region of subduction olcanics. Journal of Geophysical Research, 97: 2037 -2070
[28] D ez Balda MA, Mart nez Catal n JR, Ayarza Arribas P. 1995. Syncollisional extentional collapse parallel to the orogenic trend in a domain of steep tectonics: the salamanca Detachment Zone ( Central Iberian Zone, Spain ). Journal of Structural Geology, 17: 163 - 182
[29] D\'Lemos, R. S. D. , Brown, M. and Strachan, R. A. , 1992, Granite magma generation, ascent and emplacement within a transpressional orogen. J. Geol. Soc. London, 149:487-490
[30] England PC, Thompson AB. 1984. Pressure-temperature-time paths of regional metamorphism. I. Heat transfer during the evolution of regions of thickende continental crust. J. Petrol. , 25:894 -928
[31] England PC, Thompson AB. 1986. Some thermal and tectonic models for curstal melting in continental collision zones. In: Coward M P, Rice A C. (eds) Collision Tectonics. Geological Society, London,Special Publication. , 19:83 -94
[32] Faure G. 1986. priciples of Isotope Geology(2nd. ). New York: John Wiley and Sons, 1 -589
[33] Gao ZJ, Peng CW. 1985. The precambrian of Tianshan, Xinjiang.Xinjiang Geology, 3 ( 2 ): 14 - 25 ( in Chinese)
[34] Gill JB. 1981. Orogenic andesites and plate tectonics. Springer-Verlag,New York, 1 - 390
[35] ten Grotenhuis S. M, Trouw R. A. J. , Passchier C. W. , 2003. Evolution of mica fish in mylonitic rocks. Tectonophysics, 372:1 -21
[36] Gu LX, Yang H, Yan ZF, Liao JJ, Wang JZ. 1990. Rb-Sr geochronology and the tectonic evolution of the east section of the Middle Tianshan Mountains. Journal of Guilin College of Geology,10:49 -55 (in Chinese)
[37] Gu LX, McClay KR. 1994. Pressure solution of sulphides in some massive sulphide zine-lead deposits of western Canada:ore-forming materials. Chinese Journal of Geochemistry, 13 (2) :132 -139
[38] Gu LX, Hu SX, Chu Q, Yu CS, Xiao XJ. 1999. Pre-collision granites and post-collision intrusive assemblage of the Kelameili-Harlik orogenic belt. Acta Geologica Sinica (English edition), 73(3) :316- 329
[39] Gu LX, Gou XQ, Zhang ZZ, Wu CZ, Liao JJ, Yang H, Yiin L and Min MZ. 2003. Geochemistry and petrogenesis of a multi-zoned high Rb and F granite in eastern Tianshan. Acta Petrologica Sinica, 19(4):585 -600 (in Chinese with English abstract)
[40] Handy MR, Franz L, Heller F, Janott B, Zurbriggen R. 1999. Multistage accretion and pexhumation of the continental crust ( ivreacrustal section, Italy and Switzerland). Tectonics, 18: 1154- 1177
[41] Harris N B W, Inger S. 1992. Trace element modeling of pelite-derived granites. Contrib. Mineral. Petrol. , 110:46 - 56
[42] Harris N, Massey J. 1994. Decompression and anatexis of Himalayan metapelites. Tectonics, 13: 1537 - 1546
[43] Harrison TM, Lovera OM, Grove M. 1997. New insight into the origin of two contrasting Himalayan granite belts. Geology 25:899 -902
[44] Henderson P. 1984. General geochemical properties and abundances of the rare earth elements. In: P. Henderson ( ed. ), Rare Earth Element Geochemistry, Armsterdam: Elsevier Science Publishers. 1-32
[45] Hodges KV, Burchfiel BC, Royden LH, Chen Z, Liu Y. 1993. The metamorphic signature of contemporaneous extension and shortening in the central Himalayan orogen: data from the Nyalam transect,southern Tibet. Journal of Metamorphic Geology, 11:721 -737
[46] Hu A Q, Wang Z G, Tu G C. 1997. Geological Evolution, Petrogenesis and Metallogeny of North Xiinjiang. Beijing: Science Press, 1 -246( in Chinese)
[47] Hu A Q, Jahn B M, Zhang G X, Chen Y B, Zhang Q F. 2000. Crustal evolution and phanerozoic crustal growth in northern Xinjiang: Nd isotopic evidence. Part Ⅰ. Isotopic characterization of basement rocks. Tectonophisics, 328:15 -51
[48] Hu AQ, Zhang GX, Chen YB, Zhang QF. 2001. A model of division of the continental crust basement in the Xinjiang-based on studies of isotope geochronology and geochemistry. Xinjiang Geology, 19 (1):12 - 19 (in Chinese)
[49] Hu B, Wang JB, Gao ZJ, Lu Q, Fang XT. 1964. Several problems of tectonic evolution in Xinjiang. Acta Geologica Sinica. 44 (2): 156 -170 (in Chinese)
[50] Hu L 1998. An Intruduction to Microtextures. Geological Publishing House. 1 - 158(in Chinese)
[51] Hu SX, Ling QL et al. , 1988. The geology and metallogeny of the amalgamation zone between ancient North China and South China plate (Taking Qinling Tongbai as an example). Publishing House of Nanjing University, 1 - 588 ( in Chinese)
[52] Hu SX, Guo JC. 1989. A comparison between the autochthonous and parautochthonous transformation type granitoids in East Qinling and South China Caledonian Fold Belts. Acta Petrologica Sinica, 1: 50- 58 ( in Chinese)
[53] Hu SX, Guo JC, Gu LX. 1990. Geology of the Caledonian orogenic belt and its importance to the framework of East Tianshan ( E 85 ~ 95°) .Geoscience of Xinjiang, Geological Press, Beijing, 1: 32 -45 ( in Chinese)
[54] Inger S, Harris N. 1993, Geochemical constraints on leucogranite magmatism in the Langtang Valley, Nepal, Himalaya. Journal of Petrology 34:345 368
[55] Inger S. 1994. Magma genesis associated with extension in orogenic belts: exaples from the Himalayan and Tibet. Tectonphysics, 238:183 - 197
[56] Institute of Geology, Chinese Academy of Sciences. 1959. Tectonic of Outline of China. Science Press, 1 -320 (in Chinese)
[57] Jung S, Hoernes S, Masberg P, Hoffer E. 1999. The petrogenesis of some migmatites and granites ( central Damara orogen, Namibia ):evidence for disequlibrium melting, wall rock contamination and crystal fractionation. J. Petrol. , 40:1241 - 1269
[58] Kebede T, Koeberl C, Koller F. 2001. Magamtic evolution of the SuqiiWagga garnet-bearing two-mica granite, Wallagga area, Western Ethiopia. J. Afr. Earth. Sci. , 32 (2) :193 -221
[59] Kroll H, Schmiemann I, C? lln GV. 1986. Feldspar solid solutions.Amer. Geol. , 71:1 - 16
[60] Le Fort P, Cuney M, Deniel C, France-Lanord C, Sheppard, SMF,Upreti BN, Vidal P. 1987. Crustal generation of the Himalayan leucogranites. Tectonophysics, 134:39 - 57
计量
- 文章访问数: 8234
- PDF下载数: 5945
- 施引文献: 0