“graben”可以造什么句，graben造句

A graben creates a favourable setting for uranium deposition.

The Fuxin basin is a late Mesozoic NNE-trending graben coal-bearing basin.

The Shulan basin is located in the middle sector of Yilan-Yitong rift, and is a semi-graben basin.

The fourth phase is that the NS graben structure was produced by EW expanding mechanism in late Cenozoic.

In a half-graben, the early-stage movement of the basin-controlling Fault results in a great height difference along the lake margin.

A two dimensional non-linear finite element scheme was used in the study of stress field on a deep section of a typical graben system.

Between graben are relatively high-standing blocks called horsts.

The Datong Basin is an unsymmetrical graben, the main controlling fault of which runs north east.

The Xinding basin in the north of Shanxi rift system is a normal fault-controlled extensional graben and has a strong neotectonic process during the Quaternary.

The structural styles of the basins in early stage are all half-graben depression and in late stage are total-reverse thrust nappe and semi-reverse normal- or abnormal-reverse structures.

There are three models of ground subsidence: cave in ground subsidence, sink ground subsidence and graben ground subsidence.

Taiyuan, a city situated in Fen-Wei graben geothermal zone, is rich in geothermal resources.

Faults styles are mainly graben and step fault. Strata are little folded. Strata thickness and buried depth both decrease eastward and northward.