论文部分内容阅读
板块构造学说问世以来,不少人对传统的沉积理论提出了各种评论。迪茨和霍尔登(1966)提出用冒地斜(miogeocline)概念取代经典的冒地槽,R.H.Dott,Jr(1974)则认为前人对地槽的认识好象印度寓言“瞎子摸象”一样只看到局部而没有看到整体,A.H.Mit-chell 和 H.C.Reading(1966),C.K.Seyfert 和 L.A.Sirkin(1973)认为地质历史时期的沉积作用基本上和现代一样,主要是大陆边缘沉积。许多沉积环境和沉积类型用板
Since the advent of plate tectonics, many people have put forward various comments on the traditional depositional theory. Diez and Holden (1966) proposed to replace the classic sabotage with the concept of miogeocline (RHDott, Jr. (1974), which suggests that the previous understanding of the sag was as if the Indian allegory " Seemingly partial without seeing the whole, AHMitchell and HCReading (1966), CKSeyfert and LASirkin (1973) argue that the sediments in the geologic history are basically the same as the modern ones, mainly the continental margin deposition. Many depositional environments and sedimentary types of plates