rifting

The five evolution stages are developed in the Paleo-Asia ocean plate: ① rifting ( Pt2);

古中亚洋板块有5个演化阶段：①裂谷阶段（Pt2）；

Multi-episodic rifting and inverted tectonism caused complicated structural styles and geology structure.

多期裂陷和反转构造作用的叠加导致了相对复杂的构造格架样式和盆地地质结构.

The structural belt Mountain Funiu consists of the Luonan-Luanchuan rifting zone and the Shirenshan block.

伏牛山北麓构造带包括洛南 - 栾川断裂带和石人山地块.

Corresponding to three tectonic evolution stages of rifting, transition and thermal depression undergone in Lower Congo Basin, continental, evaporite and marine sequences deposited.

油田所在的下刚果盆地主要经历了裂谷期、过渡期和热沉降期三个阶段的构造演化，相应沉积了裂谷期陆相地层、过渡期蒸发岩层和热沉降期海相地层。

The tectonic evolution and petroleum geology are characterized by that ① Laiyang period is dextral pull-apart rifting stage mainly formed source rocks;

胶莱盆地构造演化及油气地质特征是：莱阳组沉积期为右行走滑拉分裂谷阶段，是主要的生油岩形成期；

Though Cenozoic link dextral pull apart rift system in the northwest Pacific margin basically inherited their original tectonic framework in post rifting period, they underwent some reformation, especially the Philippine Sea Basin.

西北太平洋边缘形成连锁右行拉分裂谷系统后，在后裂谷期它们虽然基本上继承了原来盆地格架，但遭到一定程度的改造。

below daka there is a hiccup in the geological succession where the vagaries of rifting and erosion have deleted a hunk of time.

这里似乎是地质序列上的一处异类，裂谷和侵蚀等奇特地表仿佛被时间长河统统抹去。

Tectonic activities controlled basin type, subside central rifting, source rock distribution, oil and gas migration and accumulation as well. Furthermore, it controlled trap formation and petroleum distribution.

研究区的构造活动不仅控制了沉积盆地类型和沉降中心的迁移，而且控制了烃源岩的分布、油气运移和聚集，还影响了圈闭的形成和油气分布。

The Cretaceous is an intraplate-rifting stage, characterized by representative geological elements such as AA-type granite, red down-faulted basins, bimodal subvolcanic rocks and basic volcanic rocks.

白垩纪为陆内裂谷阶段，形成的代表性地质要素有AA型花岗岩、大量陆相红色断陷盆地、基性火山岩、双峰式次火山岩等。

The paleo rifting ( taphrogeny) controls the development of the volcanic belt and at the same time it is favourable metallogenic tectonic environment;

古裂谷（或裂陷）既控制了火山岩带的发育，又是有利的成矿构造背景；

The original types of unconformity surface of Zhanhua trough include unconformity of basement, unconformity of episodic rifting and unconformity of break, as well as the unconformity or break related to tectonic movement, water level change, sedimentary process and climate change.

沾化凹陷的不整合成因类型包括基底不整合、裂陷幕不整合、破裂不整合和与构造活动、水位变化、沉积过程及气候变迁相联系的不整合或沉积间断。

The eastern China Continent has entered into the stage of rifting continental margin since Oligocene.

自渐新世,中国东部大陆进入了张裂的大陆边缘阶段.