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喜山

网络Yoki-san; MountPleasant

喜山

喜山

Yoki-san

...流(Ryoku-ryu) 箕轮(Miniwa) 与喜山(Yoki-san) 榛原红(Haibara-beni) 摺墨(Suru-sumi) 瑞穗红(Mizuho-Beni) 舞孔雀(Mai-kujaku…

MountPleasant

...MichiganUniversity ）、位於图喜山（MountPleasant ）的中密西根大（学 CentralM ichiganUniversity ）、以及位於图奎 …

1

The reservoirs were uplifted to be exposed and be denuded and were changed into the present oil sands finally during the Himalayan movement .

进入喜山运动，早先形成的油藏抬升暴露、剥蚀而最终形成了目前的油砂矿体。

2

During the Himalayan period, fold and superimposed deformation had been happened, and cased preexisting structure reformed .

喜山期发生褶皱叠加并进一步改造先期构造。

3

Late Indosinian and Himalayan progenies reformed and destroyed them , but are favorable for the formation of continental petroleum systems .

印支晚期一喜山期造山作用对其具有改造和破坏作用，但利于陆相含油气系统的形成。

4

The first anticline zone formed Triassic oil reservoirs in Indosinian period and formed Jurassic reservoirs in Himalayan period .

第一排背斜带于印支期形成三叠系油藏，喜山期形成侏罗系油藏。

5

Middle and late Himalayan movements determined the formation and development of structural traps.

喜山运动中晚期活动控制构造圈闭的形成和发展；

6

The tectonic stress field in Chengdao area of Yanshan and Himalaya periods is simulated with finite element method .

用有限元法模拟了埕岛地区中、古生界燕山、喜山两期构造应力场。

7

Anxian movement and cross-formational flow in Himalayan stage are important factors to form good sandstone reservoirs .

安县运动及喜山期的流体跨层流动对形成良好储层具有重要作用。

8

not the structure of solid minerals filling fractures formed in the Himalayan period . 2.

未被固体矿物充填的构造裂缝，形成于喜山运动时期。

9

Ore ~ forming is connected to mantle fluid in the Himalaya stage and it plays essential r. . .

成矿与喜山期地幔流体的活动有关，它在成岩成矿过程中起主导作用。

10

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