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   构造-沉积旋回 的翻译结果: 查询用时:0.188秒
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构造-沉积旋回
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     “L-STRUCTURE”FOR FUZZY SET IN A LINEAR SPACE
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According to the basic comception of tectostratigraphy,the author divided the Meso-Cenozoic Systems in East China into six tectonic-sedimentary cycles and proposed that theLower Eogene should belong to Upper Cretaceous,Upper Triassic to Lower Jurassic inSouth China and the Nanyang Basin to Cretaceous.An important tectonic generation inthe end of Jurassic is significant in dividing the tectonic evolution history into two stages,that is,Triassic-Jurassic stage and Late Cretaceous-Tertiary stage.Two huge tectonic...

According to the basic comception of tectostratigraphy,the author divided the Meso-Cenozoic Systems in East China into six tectonic-sedimentary cycles and proposed that theLower Eogene should belong to Upper Cretaceous,Upper Triassic to Lower Jurassic inSouth China and the Nanyang Basin to Cretaceous.An important tectonic generation inthe end of Jurassic is significant in dividing the tectonic evolution history into two stages,that is,Triassic-Jurassic stage and Late Cretaceous-Tertiary stage.Two huge tectonic sys-tems that developed in the stages derived from the same origin but different from eachother.Extensive tectonic uncomformities could be found between the tectonic systems,thus resulting in two dimensional feature of Meso-Cenozoic Systems in East China.

根据构造地层学的原理和方法,将中国东部中、新生界划分为六个构造-沉积旋回,认为侏罗纪末幕运动是中、新生代最重要的、具有划分构造发展阶段意义的构造幕,从而把中、新生代构造演化史划分为三叠-侏罗纪、晚白垩世-第三纪两个阶段和早白垩世过渡阶段,并概述了每个阶段的基本构造特征。

The Zanda basin, bounded by the Ayila Ri'gyu and Boling faults in the northeast and southwest respectively, is located in the southwest of the Tibetan plateau. There developed a suite of Pliocene to Pleistocene strata, which can be, from bottom to top, divided into four members: A, B, C and D. The first three members, representing three large tectonic cyclothems, have similar sedimentary features. Their lower parts are composed of conglomerates deposited in braided river, the sandstones of middle parts deposited...

The Zanda basin, bounded by the Ayila Ri'gyu and Boling faults in the northeast and southwest respectively, is located in the southwest of the Tibetan plateau. There developed a suite of Pliocene to Pleistocene strata, which can be, from bottom to top, divided into four members: A, B, C and D. The first three members, representing three large tectonic cyclothems, have similar sedimentary features. Their lower parts are composed of conglomerates deposited in braided river, the sandstones of middle parts deposited in meandering river, and the upper parts being lacustrine mudstones with minor thin sandstones. The member D is a suite of lacustrine mudstone. Cyclothemic characteristics, penecontemporaneous and subsequent deformation reflect that this area was compressed, from Pliocene, by the regional stress, and uplifted strongly. What mentioned above provided strong support for the Tibetan uplifting in the recent several million years.

札达盆地位于青藏高原南西部 ,其北东和南西侧分别为阿依拉日居和波林断裂系所限。在盆地内沉积了一套上新世 -更新世地层 ,从下至上可分四段 ,上部为湖相泥岩段 ,下部三段代表了三个构造沉积旋回 ,它们有类似的沉积特征 ,即 :每段下部为辫状河沉积的砾岩层 ,中部主要为曲流河沉积的砂岩层 ,并逐渐过渡到上部湖相泥岩。旋回沉积特征和地层变形反映了本区从上新世以来处于挤压状态 ,并有强烈垂向运动 ,为青藏高原在近几个百万年来持续隆升提供了依据。

Post-reformation is one of the most typical characters of the petroliferous basins of China compared with those of the world.It strongly affects hydrocarbon generation,pool-forming and the preservation of oil and gas resources.In turn,the post-reformation is closely related to the inherent geological features of the petroliferous basins of China.The formation of petroliferous basins relied mainly on the broken landmasses or micro-continents.In the global tectonic evolution,they were placed in between the surrounding...

Post-reformation is one of the most typical characters of the petroliferous basins of China compared with those of the world.It strongly affects hydrocarbon generation,pool-forming and the preservation of oil and gas resources.In turn,the post-reformation is closely related to the inherent geological features of the petroliferous basins of China.The formation of petroliferous basins relied mainly on the broken landmasses or micro-continents.In the global tectonic evolution,they were placed in between the surrounding macro-oceanic plates in Palaeozoic,and in between the Siberian and Indian continental plates and several oceanic plates in Pacific since Mesozoic.Their multi-separation and aggregation as well as formation and evolution were always controlled by the stress accumulation and dissiplation of the geodynamic systems of the surrounding plates,thus resulting in the unique features of multi-stage basin-formation and multi-superposition of different stage basins,the multicyclic tecto-sedimentary evolution and multiple post reformation of the basins.

成盆期后改造是中国含油气盆地与世界相比最具个性特色的一种构造现象 ,它对盆地的成烃、成藏和油气资源的保存程度影响至深。而成盆期后改造又与中国含油气盆地的固有地质特征密切相关。中国含油气盆地的形成主要以微小的破碎陆块为依托。在全球构造演化中 ,古生代它们被夹持于周围巨大的大洋板块之间 ,中生代以来则夹持于同样巨大的西伯利亚、印度大陆板块和太平洋诸大洋板块之间。它们的多次分离和聚合 ,以及由此导致的盆地形成和演化始终处于周围板块动力系统应力积聚和消散的制约之中 ,由此造就了中国含油气盆地多期成盆、不同期盆地多次叠加、多构造沉积旋回演化和多次成盆期后改造等独有特色。

 
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