The geochemical characteristics of those stable elements mentioned above show that pillow lavas fro.
河南省西峡县二郎坪群绿片岩相枕状熔岩岩枕保存完整,受构造改造轻微。
Based on the Middle-Late Paleozoic pillow lava and Permian-Triassic tectonic melange, this paper shows that there is a melange zone along Qinzhou-Cenxi-Luoding-Yunfu.
作者等在两广交界罗定一带新发现了中晚古生代的枕状熔岩和二叠—三叠纪的构造混杂岩,结合区域构造,分析并提出了钦州-岑溪-罗定-云浮构造混杂带的存在。
Pillow structure and ball-and-pillow structure are the soft-sediment deformation within strata.
枕状构造(pillow)与球—枕构造(ball-and-pillow)、负载构造(load))是地层中的软沉积物变形构造,它们在形态、产状、变形机制等方面是不同的。
