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對(duì)韌性剪切帶形成深度和變形環(huán)境研究方法與研究?jī)?nèi)容及想法-資料下載頁(yè)

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【正文】 剪切帶研究及其地質(zhì)意義,地球科學(xué)進(jìn)展。Vol 20。No7[7]陳柏林等,1999韌性剪切帶型金礦成礦模式,地質(zhì)論評(píng),Vol 45。No2[8],巖石磁組構(gòu)在構(gòu)造混雜巖帶研究中的應(yīng)用—以西天山地區(qū)為例,地球物理學(xué)進(jìn)展,Vol 13。No1[9]聶江濤等,[10]陳意等。2004,韌性剪切帶中片麻巖和超高壓榴輝巖8001200米巖心的證據(jù)。巖石學(xué)報(bào) Vol 20. No1[11]AbdelRahman Fowler The significance of gneissic rocks and synmagmatic extensionalductile shear zones of the Barud area for the tectonics of the North Eastern Desert, Egypt. Journal African Earth science 201220[12]Eric C. Ferr233。 and magnetic fabrics in ductile shear zones: A .. of page 10[13]Nibir Mandal etc,Problem of folding in ductile shear zones,a theoretical and experimental of Structural Geology 26 (2004) 475–489[14], 2001,strain in ductile shear zones in the Caledonides of northern Sweden a threedimensional puzzle 23(2001)15491565[15].Cao J M, Zhu J S, Wu D , Velocity structure of the crust in east ern Qinling mountain[ J] . Journal of C hengdu Inst itut e of Technology, 21( 1) : 1117( in Chin ese) .
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