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作 者:陶宗普[1] 唐东[2] 江春明[1] 苏宗富[1] 王胜建[1]
机构地区:[1]中国地质大学能源学院,北京100083 [2]中石化胜利油田地质院,山东东营257000
出 处:《重庆科技学院学报(自然科学版)》2005年第3期26-28,共3页Journal of Chongqing University of Science and Technology:Natural Sciences Edition
摘 要:沉积残留物是指原始沉积体系的沉积物在沉积后受到侵蚀,普遍意义上指沉积的准同时受到侵蚀而保留下来的那部分残留物。沉积残留物可形成于沉积物未固结时,因而会与高级别的层序边界和水进不整合,与低级别的层序边界不整合伴生。强调沉积残留物是准确确定原始沉积,避免误解沉积分布,有效地指导隐蔽圈闭的勘探和开发。Depositional remnants is a stratigraphic term put forward and elaborated systematically by R.S. Martinsen etc. And the term means a sedimentary deposit that is only part of an original depositional system preserved after subsequent, but commonly penecontemporaneous erosion. Consequently, the depositional remnants may form while the deposits are still unconsolidated and so it may develop in association with high-order sequence-bounding and transgressive unconformities as well as low-order sequence-bounding unconformities. This paper argues that depositional remnants is beneficial to accurate confirmation of original deposits, avoiding of making mistakes in sedimentary distribution, effective guiding of the subtle-trap exploration and development. Thus the term should be highlighted by petroleum geologists.
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