The author define the diwa-type orogeny in the frame of diwa theory as the collection of geological processes wlthin post-platformal tectono magmatism, and then divide it by the manifestations and dynamics of crustobody into three sub-types, convergent, divergent and hybrid diwa-type oro.
笔者将地洼型造山运动定义为在后地台构造-岩浆活化过程中各种地质作用的总称，并且依据壳体运动的方式和力源，可以将地洼型造山运动划分为离散式、汇聚式和混合式三类。
Volcanic eruptive belts from Ningguo to Cuomai is divided into two volcanic tectonic depression including Ningguo and De.
根据区域构造背景、火山岩地层时空分布特征、岩性、岩相及喷发形式,将研究区划分为三个火山喷发带,其中宁果—措麦火山喷发带又可划分为宁果和德诺两个火山构造洼地,卢当—查孜火山喷发带划分为孔隆—邦勒、松拉勒—腊尔格和孔驹密波—查孜三个火山喷发亚带。
