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一、基本地质特征渤东潜山带原名中央构造带。现已查明:它是位于渤中凹陷和辽东、渤东凹陷之间的一个北北东向地垒状潜山带,是辽东潜山带向南的延伸部分。渤东潜山带的地质构造具有自己活动规律和表现形式。从区域地质背景上看,应归属郯芦断裂带中的组成部分。首先,表现在构造形态特征是一个地垒状和狭长胡同状的块断潜山带,北段是由四组平行断层构成的两级地垒,最高部位处于中央,中段基本由两条断层组成的单一地垒,顶部平宽,仅于东侧局部形成高垒块状隆起;南段,由地垒状过渡到西断东倾的单断形
First, the basic geological features Bodong buried belt formerly known as the central tectonic belt. It has been ascertained that it is a north-north eastward basement buried hill belt located between the Bozhong Sag and the Liaodong and the Bodong Depression and is an extension of the southward extension of the Liaodong buried hill belt. The geological structure of the Bodong buried hill has its own rules of activity and manifestation. Judging from the regional geological background, it should be attributed to the components of the Rulu fault zone. First of all, the tectonic features are block-shaped and narrow alluvial block fault buried mountain belt. The northern segment is a two-level basement consisting of four parallel faults. The highest part is in the center and the middle part is composed of two faults Of the single base, the top of the flat, only in the eastern part of the formation of high-rise massive bulge; the southern section,