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Studies of the evolution and changes in the Tethys Ocean occurring during past 200 Ma may provide a model for fut...

在对藏南白垩纪沉积地质详细研究基础上,本文对尼泊尔喜马拉雅和Lhadkh喜马拉雅白垩系进行了对比。

in this paper can be summarized as follows: 1 Based on the Zongshan Section of Gamba and the Chuangde Section of Gyangze in southern Tibet, three Upper Cretaceous units have been recognized as black, gray and red ones.

本论文主要得出了以下几点认识: 1由西藏南部晚白垩世的岗巴宗山剖面和江孜床得剖面可以识别出三套岩层:黑层段,灰层段和红层段。

The Gamba basin of southern Tibet, is located in the east of Tethys tectonic region, whereexposes complete strata from late Cretaceous to Paleogene. The strata yield abundantfossils, and accurate biostratigraphic works have been done by previous studies.

西藏南部岗巴盆地位于位于特提斯构造域的东端,发育有完整的晚白垩世至古近纪地层,地层中化石丰富,前人根据化石研究准确地进行了地层时代的划分。

Foraminiferal fauna ; Recovery ; Late Cretaceous ; Gamba ; Tibet

有孔虫动物群;生物复苏;晚白垩世;岗巴;西藏

Then the wolf went to the grocery store, and brought a big piece of gesso.

于是,狼跑到杂货商那里,买了一大块白垩土,吃了下去,结果嗓子变细了。

The lithologic pool such as that developed in the actic region while the basin is rifting or in the glacis region while the basin is depressing all which can be found in this basin. Five kinds of sedimentary facies and thirteen sedimentary parfacies can be found in the Shengbei concave during the period of Jurassic series and Cretaceous series.

在该盆地内部既有可能发育断陷期陡坡带的岩性油气藏,又有可能发育坳陷期缓坡带的岩性油气藏,其胜北洼陷在中侏罗统-白垩系沉积时期主要发育5种陆相沉积相类型、10种沉积亚相类型。

The distribution and its forming condition of sporepollen fossil resedimented inTertiary system in Yilan-Yitong graben are throughly analyzed in this paper.

本文对依兰-伊通地堑第三系再沉积孢粉化石的分布及其形成条件进行了深入的分析,提出了再沉积的孢粉化石来自晚白垩世地层及其主要的鉴别方法。

All these were led by Idomeneus, and by Meriones, peer of murderous Mars.

鲁克托斯、米勒托斯和白垩闪亮的鲁卡斯托斯。

In working area and its adjacent area, the forming tectonic setting of Indosinian intrusion was that orogenic belt pressed strongly, intracontinental subduction; that of early Yanshan movement epoch was the stress field transferred from compression to extension meanwhile the incrassate crust of orogenic zone turned to extensional collapse; and that of early Cretaceous volcanics was that the area structure extensional collapse further more during the post period of orogenic phase.

研究区及邻区印支期侵入岩形成于造山带强烈挤压陆内俯冲的构造环境;燕山早期侵入岩形成于由挤压转向拉伸、造山带的增厚陆壳开始发生伸展垮塌的构造环境;早白垩世火山岩形成于造山期后进一步发生伸展垮塌的区域构造环境。

Affeted by transgression, three times of lake ingression occured and formed three sets of source rocks of salty enviroment in Subei basin.

受海侵影响,苏北盆地在晚白垩世至古新世曾发生三次湖泛,形成三套半咸化环境的烃源岩系。

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