CAJ | 학술논문

在对地质资料、地震资料及地球化学资料详细解剖的基础上，以东营凹陷西部红层沉积期构造演化阶段的划分及古地貌的恢复为切入点，通过对物源、沉积体系的系统研究，明确了东营凹陷西部红层沉积期物源方向及沉积体系的时空演化特征。研究认为：东营凹陷西部红层沉积期可以划分为孔一段时期和沙四下亚段时期两个构造演化阶段；红层沉积前盆地整体呈现四面环凸、西高东低、西部地形整体较为平缓的古地貌格局，古地貌的时空差异影响并控制了东营凹陷西部红层层系的沉积。东营凹陷西部红层沉积期存在西北无棣-滨县凸起和南部鲁西隆起两大远物源体系和平南断层上升盘近物源体系，红层沉积后期，平南断层上升盘近物源体系消失。东营凹陷西部红层沉积期主要发育了冲积扇、辫状河、湖泊及滩坝等沉积体系，盆地北部还发育了近岸水下扇沉积体系；古地貌、古物源及古气候的变迁使得沉积体系的时空展布表现出继承性与差异性并存的特征。
재대지질자료、지진자료급지구화학자료상세해부적기출상，이동영요함서부홍층침적기구조연화계단적화분급고지모적회복위절입점，통과대물원、침적체계적계통연구，명학료동영요함서부홍층침적기물원방향급침적체계적시공연화특정。연구인위：동영요함서부홍층침적기가이화분위공일단시기화사사하아단시기량개구조연화계단；홍층침적전분지정체정현사면배철、서고동저、서부지형정체교위평완적고지모격국，고지모적시공차이영향병공제료동영요함서부홍층층계적침적。동영요함서부홍층침적기존재서북무체-빈현철기화남부로서륭기량대원물원체계화평남단층상승반근물원체계，홍층침적후기，평남단층상승반근물원체계소실。동영요함서부홍층침적기주요발육료충적선、변상하、호박급탄패등침적체계，분지북부환발육료근안수하선침적체계；고지모、고물원급고기후적변천사득침적체계적시공전포표현출계승성여차이성병존적특정。
Based on the detailed analysis of geological data,seismic data and geochemical data,through the method of the dividing of structure evolution stages and recovery of palaeogeomorphic,combined with prove-nance sedimentary system,the paper studied the temporal and spatial evolution features of sedimentary system and provenance orientation in the red-bed sedimentary period in the western area of Dongying Sag.The period in the western area of Dongying Sag was divided into the 1 st of Kongdian Formation and the lower part of the 4th member of Shahejie Formation.Before deposition of the 1 st member of Kongdian Formation,the Luxi uplift, Guangrao bump,Chenjiazhuang bump,Binxian bump and Wudi bump were formed.The main faults are Chen-nan Fault,Binnan Fault,Yangxin Fault,Shicun Fault and Gaoqing-Pingnan Fault and so on.The whole basin presents the palaeogeomorphic of bumps around,east low,and west high and flat terrain in the west.The prove-nance of the western area of Dongying Sag in the early stage of Kongdian-Shasi is mainly from the northwest and the south orientations.There are two further provenance systems of Wudi to Binxian bump,Luxi uplift,and one provenance system of Pingnan Fault.There are sedimentary systems such as alluvial fan-braided river-lake sys-tem,alluvial fan-alluvial plain-lake system,lake-beach bar and subaqueous fan-lake system.The changes of palaeogeomorphic,provenance and ancient climate influence the temporal and spatial evolution of the sedimen-tary system with the characteristics of inheritance and difference.