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机译:高岭土多态性证据表明,在欧洲陷的裂谷过程中,沿着加里东冲断带有热流体脉冲
Department of Geology, University of Aberdeen, Aberdeen AB24 3UE, UK;
Department of Geology, University of Aberdeen, Aberdeen AB24 3UE, UK;
Department of Geology, University of Aberdeen, Aberdeen AB24 3UE, UK;
Department of Geology, University of Aberdeen, Aberdeen AB24 3UE, UK;
Scottish Universities Environmental Research Centre, East Kilbride G75 0QF, UK;
School of Geology & Geophysics, University of Oklahoma, Norman, OK 73019, USA;
School of Geology & Geophysics, University of Oklahoma, Norman, OK 73019, USA;
School of Geology & Geophysics, University of Oklahoma, Norman, OK 73019, USA;
Geotrack International Pty Ltd., 37 Melville Road, Brunswick West, Victoria, Australia;
kaolin; polytype; Caledonian; European margin; Moine thrust; dickite; hematite;
机译:高岭土多态性证据表明在欧洲Mar陷的裂谷过程中沿喀里多尼亚冲断带有热流体脉冲
机译:新特提斯人的阿拉伯被动大陆边缘的侏罗纪早期裂谷。伊朗扎格罗斯褶皱冲断带的卢尔斯坦地区的现场证据
机译:穆尼推力区Achnashellach凝结过程中的卡利多前断层证据:推力前模板在影响褶皱和冲断带发育方面的重要性
机译:在裂痕大陆边缘的热重力异常有哪些证据?
机译:褶皱-冲断系统覆盖了倒裂盆地边缘的同裂谷构造:西得克萨斯州印第奥山脉。
机译:早期的侏罗纪剥夺了新人的阿拉伯被动大陆边缘。来自ZAGROS折叠和推力带,伊朗的LURESTAN地区的现场证据