1) Fangzheng fault depression
方正断陷
1.
Paleogene structural evolution and distribution characteristics of sedimentary facies in the Fangzheng fault depression of the Yishu graben;
依-舒地堑方正断陷古近系构造演化与沉积相带展布特征
2.
Fault system and tectonic pattern analyses of Fangzheng fault depression
方正断陷断裂系统与构造样式
3.
Sedimentary characteristics of Xin'an village group's 3D seismic zone in Fangzheng fault depression
方正断陷三维区新安村组沉积特征
2) Fangzheng Rift
方正断陷
1.
Description of Structure-Conglomerate Gas Reservoir in Fang3 Well Area of Fangzheng Rift;
方正断陷方3井区砂砾岩构造气藏描述
2.
Based on the negative flower shaped structure and its relative structural movement track in Fangzheng area,this paper suggests that Fangzheng Rift is a rifted basin formed by strike slip pull apart.
本文通过对方正地区所发现的负花状构造及其有关构造运动形迹分析的基础上,进一步提出方正断陷是走滑—拉分形成的断陷盆地。
3.
0 metre in the Fangzheng Rift, northeast of the Yilan-Yitong Rift Valley.
依兰—伊通地堑方正断陷方参 2井 2 10 4。
3) Fangzheng fault
方正断陷
1.
According to core,seismic,well log and logging data,utilizing the principles and methods of sequence stratigraphy and sedimentology to identify the sedimentary micro-facies characteristics of Xin an village group in Fangzheng fault area of yishu graben.
依据岩心、地震、测井和录井资料,应用层序地层学和沉积学的原理和方法,查明了伊舒地堑方正断陷新安村组沉积微相特征。
4) fault depression
断陷
1.
Structural characteristics of deep fault depressions in the southeastern uplift area of the Songliao basin,China and their significance for petroleum exploration;
松辽盆地东南隆起区深层断陷的构造特征及其对油气勘探的意义
2.
Characters of reverse tectonics and its forming mechanism in late of fault depression in Songliao basin.;
松辽盆地断陷末期反转构造特征与形成机制
3.
The fault depressions,isolated with one another but genetically related,are developed in deep of southern Songliao basin and most of them are considered to be capable of generating hydrocarbon.
松辽盆地南部深层系发育了既相互分割又有成因联系的断陷群,多具有生烃能力。
5) rift
[英][rɪft] [美][rɪft]
断陷
1.
This paper analyzes the gas reservoir formation condition of all the rifts in the north part of Songliao Basin, and proposes the apparent difference of hydrocarbon source rock development, organic matter evolution and cap rock condition among the rifts.
在深入分析松辽盆地北部各断陷天然气成藏条件的基础上 ,指出各断陷在烃源岩发育、有机质演化程度和盖层条件上存在明显的差异。
2.
It determines that Xujiaweizi Rift is a complex rift controlled by two large fractures,i.
利用综合勘探程度较高的松辽盆地徐家围子断陷钻井与地震资料,对早白垩世早期(相当于热河生物群时代)的地层进行了构造特征研究。
3.
This paper discusses the effect of tectonics such as uplifting of the asthenosphere in the deep basin,the interaction between the crust and the mantle,the net structure,crust thinning and the detaching zone on the forming and evolving mechanism of the shallow rift and faults,providing.
探讨了盆地内深部的软流圈上隆、壳—幔相互作用、拖网结构、地壳减薄、拆离带等地质作用对浅部断陷和坳陷的形成和演化的控制机理。
6) square runner
正方断面流道
补充资料:断陷盆地
断陷盆地
指断块构造中的沉降地块,又称地堑盆地。它的外形受断层线控制,多呈狭长条状。盆地的边缘由断层崖组成,坡度陡峻,边线一般为断层线。随着时间的推移,在断陷盆地中充填着从山地剥蚀下来的沉积物,其上或者积水形成湖泊(如贝加尔湖、滇池),或者因河流的堆积作用而被河流的冲积物所填充,形成被群山环绕的冲积、湖积、洪积平原。如太行山中的山间盆地和地堑谷中发育着的冲积洪积平原。低于海平面的断陷盆地被称为大陆洼地。
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参考词条