1、

Forming during Yanshanian period and influenced by the basement tectonics, the main structure styles in the research area are subdivided into three types& compressive fault block, extensional fault block, and thrust fold.

研究区主要的构造样式是在燕山期形成的,但也受到了基底构造的直接影响,所以比较复杂。其构造样式可以分为挤压块断、伸展断块、逆冲褶皱三种基本类型。

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2、

In extensional tectonic stress field, there are paralleling and ring-radiating fault block modes.

在张性应力场中常见的断块模式有平行断块模式和环状一放射状断块模式.

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3、

Sand Box Analog Models of Extensional Fault Systems

伸展断层系统的砂箱模拟实验

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4、

In extensional fault, there are a lot of fluid inclusions with bigger size of grains and wider range ratio of vapor to liquid.

张性断裂流体包裹体数量多,粒径大,气液比变化范围大,常伴随出现沸腾包裹体群;

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5、

The extensional fault systems are believed to be developed through the Cambrian, Ordovician, Early Silurian, Middle-Late Jurassic, and Paleogene.

伸展断裂系统发育于寒武纪、奥陶纪、早志留世、中-晚侏罗世和古近纪。

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6、

However, the extensional fault which had strong activities in the Eocene or even in the Paleocene, become non-activity from Neogene to Quaternary.

而盆地区的伸展断层则在始新世甚至古新世就有强烈的活动,而在新近纪一第四纪时期基本不活动。

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8、

The early extensional fault controlled the structure systems, forming a series of compound structures of horst and graben and sedimentary facies in which many early sedimentary characters on slope, such as glide deformation and clastic flow can be seen.

早期伸展断层控制了同期的构造和沉积特征,形成一系列复式地垒和地堑的结构,在斜坡带见滑动变形、碎屑流等构造现象。

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9、

The Early-Middle Jurassic strata were probably deposited in an extensional basin above the Lapeiquan fault.

早中侏罗世地层可能为拉配泉断裂之上的伸展盆地沉积.

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