浅谈深水块体搬运复合体的结构、成因分类以及识别方法

秦磊, 毛金昕, 倪凤玲, 徐少华, 李小刚, 蔡长娥, 尚文亮, 刘家恺

A Brief Introduction to Deep-Water Mass-Transport Complexes: Structures, Genetic Classifications and Identification Methods

Lei Qin, Jinxin Mao, Fengling Ni, Shaohua Xu, Xiaogang Li, Change Cai, Wenliang Shang, Jiakai Liu

图5 MTCs露头资料识别特征 (a)西爱尔兰上石炭统Ross海底，滑动体上覆平坦的水道充填[39]；(b)西班牙南部Tabernas盆地上中新统，滑塌岩地层发生一系列褶皱变形且被倾角很缓的水道充填[40]；(c)西班牙东北部始新世大陆斜坡地层中的碎屑岩[42]

Fig.5 The outcrop identification features of MTCs (a)The sliding body is filled with a flat channel in the upper Carboniferous Ross seafloor of Western Ireland[39]; (b)A series of folds and deformations occurred in the slump rock formation and were filled with water channels with very low dips in the Upper Miocene of the Tabernas Basin[40]; (c)Phototgraph of floating clasts in a thin debrite, Eoceneslope strata of Sant Llorenc del Munt, northeastern Spain[42]