摘要
通过野外和室内综合研究,本文认为晋中北晚古生代山西组是以河控作用为主、兼受潮汐作用改造的浅水三角洲沉积,并总结了浅水三角洲的沉积特点。聚煤作用主要发生在上三角洲平原泛滥盆地、下三角洲平原分流间湾充填变浅、废弃三角洲朵叶各部位发展起来的泥炭沼泽环境。
On the basis of synthetic studies of field and laboratory,the authors believe Shanxi formation in the middle-north district of Shanxi Province to be a fluvial-dominated shallow-water delta deposit system which is partly influenced by tidal water. And this paper sums up thesedimentary characteristics of shallow-water delta,Coal-accumulating process occured mainlyin the peat swamps that developed in the flcod basin of the upper delta plain,shallowed inter-distributory bay of the lower delta plain and every part of the abandoned delta lobe.
出处
《中国矿业大学学报》
EI
CAS
CSCD
北大核心
1995年第1期64-70,共7页
Journal of China University of Mining & Technology
关键词
山西组
浅水
三角洲
聚煤作用
煤系
Shanxi formation,shallow-water delta,coal-accumulating process