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Tectonic Model and Its Deformation Feature of Cenozoic in West Section of Lenghu Structural Belt, Northern Margin of Qaidam Basin 冷湖构造带西段新生界构造模型及变形特征
Lenghu structural belt 冷湖构造带
Peripheral gentle slope belt of drape structural belt of buried hill is the oil? 潜山披覆构造带周边缓坡带既是油气运移通道 ,又可形成各种圈闭类型的油气藏。
Datianchi structural belt situates in high and steep district where subterranean forms are complicated,and the formation dip angle is large, with lots of payzones. 大天池构造带位于川东高陡构造区，地腹形态复杂，地层倾角大，产层多，具有喷、漏、塌、卡、斜、毒等多种特性。
In the same structural belt,mud volcanoes occur in paternoster distribution along trend of the major fault and anticlinal zone. 泥火山构造在地震相上为不连续、弱振幅的空白反射或杂乱反射,呈柱状与围岩不整合接触。
It is considered that No. 2 sand body on T~U_ 3C of LZ21-4 structural belt has good physical character of reservoir and cap condition. 认为LZ21-4构造带的T3UC地层中的2砂体储集物性好,且盖层条件也好。
Banqiao rupture structural belt is located on the eastside of Banqiao sag, which is controlled by Banqiao and Dazhangtuo faults. 板桥断裂构造带位于板桥凹陷的东侧,受板桥凹陷和大张坨断层控制。
The Zhoukou depression is a Mesozoic-Cenozoic faulted depression that over-lies the North-China tectonic unit and the south-marginal structural belt. 周口拗陷是横跨在华北地块和华北地块南缘构造带上的中新生代断陷型拗陷。
Qianmiqiao buried hill in Banqiao structural belt of Huanghua Depression was formed by stretch-faulting on the basis of fold-obduction. 千米桥潜山构造位于黄骅坳陷北大港构造带,千米桥潜山构造是在中生代的褶皱逆冲作用的基础上经历伸展正断作用后形成的。
Malang Depression is a secondary structural belt of Santanghu Basin, Jurassic Series is the main oil and gas reservoir of the basin. 马朗凹陷是三塘湖盆地的一个二级构造带，侏罗系是盆地内主要含油层位。
The piedmont zone of the North Longmenshan is located at the fault front structural zone of buried faults of the nappe structural belt. 龙门山北段山前带处于推覆体构造带的断层隐伏前锋构造带,已发现中坝、河湾场气田和较多油气显示。
It is a NNE-strike low buried-hill draping structural belt on the Mesozoic buried hill at the last phase of Yanshan movement. 是在燕山运动末期、在中生代潜山背景上发育起来的北北东走向的下第三系低潜山披覆构造带。
Qianmiqiao buried hill in Banqiao structural belt of HuanghuaDepression was formed by stretch-faulting on the basis of fold-obduction. 千米桥潜山构造位于黄骅坳陷北大港构造带，千米桥潜山构造是在中生代的褶皱-逆冲作用的基础上经历伸展正断作用后形成的。
In the article,the charateristics of diagenetic evolution of middle and lower Jurassic reservoir in the Qiuling structural belt of the tuha Basin(i. 本文运用分析化验、储层测试等多种资料对吐哈盆地丘陵构造带中下侏罗统储的成岩演化特征进行了研究。
Suggests that the Xijir Ulan structure belt is splitting from Qiangtang massif. 说明西金乌兰构造混杂带是羌塘陆块上裂解形成的。
The paper uses log-constraint inversion technique to predict the reservoir and cap in LZ21-4 structural belt situated in the part of northern sub-sag of Liaozhong sag. 本文利用测井约束反演技术对位于辽中凹陷北洼部位的LZ21-4构造带储盖层进行了预测。
According to the analyses on structural evolution and sedimentary features,Jiangnan-Xuefeng Structural Belt and its edge possess favorable petroleum geological conditions. 通过构造演化与沉积特征分析,认为江南-雪峰构造带及周缘具备良好的成油气地质条件;
Therefore, it is predicted that the downthrow side of main fault in the strike-slip structural belt and the central uplift zone are most favourable for oil and gas accumulation. 从而可以预测，该凹陷周缘走滑构造带的主断层下降盘和中央隆起构造带是其最有利的油气聚集区带。
It is supposed that the NE structural belt along southeast margin of Hannan Massif belongs to the nappe formed after Mesozoic Era in terms of Hujiaying Nappe. 从胡家营的推覆构造可推知汉南地块东南缘北东向构造带,应属于中生代以来所形成的推覆体构造。
Lian Muqin structural belt is located at burning mountain area in Tuha basin, and between the Lu keqin accumulation zone for heavy oil and underfloor hollow zone. 连木沁构造带位于鲁克沁稠油聚集带与台北凹陷之间，地处吐哈盆地火焰山地区。