摘要
根据地层层序保存程度,将造山带地层分为无序地层体、断片地层体、有序地层体。本文认为造山带绝大多数地层体可进行沉积学的恢复。沉积学在造山带地层和岩相分析中具巨大作用,应更多强调构造与沉积学的紧密结合。
Orogenic stratigraphy can be divided into disorder, order or break stratigraphy. The authors think that most of the stratigraphy of the orogenic belts can be recovered for the studies of sedimentology and lithofacies. Sedimentology plays an important role in the analysis of orogenic stratigraphy and lithofacies, but more attention should be paid to the close relation between sedimentology and tectonics.
出处
《海洋地质动态》
2004年第5期17-19,共3页
Marine Geology Letters
基金
国家地调项目
不动泉
库赛湖幅 1 :2 5万区域地质调查项目资助
关键词
沉积学
造山带地层
地层层序
保存程度
岩相分析
stratigraphy types of orogenic belts
sedimentology
action and significance
