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中扬子
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  middle yangtze
     PHANEROZOIC TECTONIC EVOLUTION AND ITS INFLUENCE ON THE PETROLEUM SYSTEM IN THE MIDDLE YANGTZE REGION
     中扬子地区显生宙构造演化及其对油气系统的影响
短句来源
     The Lower Ordovician reef-bearing strata in the middle Yangtze platform may be divided into four II-type depositional sequences based on the principle and method of outcrop sequence stratigraphy.
     运用露头层序地层学原理与方法,将中扬子台地早奥陶世含礁地层划分为4个II型层序,并阐述了各层序的体系域特征和形成的沉积动力学机制以及海平面变化对沉积、生物迁移、生物礁及环境的控制作用。
短句来源
     Sedimentary characteristics and lithofacies palaeogeography of the Late Sinian and Early Cambrian in middle Yangtze region
     中扬子地区晚震旦世—早寒武世沉积特征及岩相古地理
短句来源
     Distribution of Strontium in Upper Sinian Corbonate Rocks along the Northern Margin of Middle Yangtze Platform and Its Environmental Implications
     中扬子台地北缘上震旦统碳酸盐岩中锶的分布特征及环境意义
短句来源
     STRATIGRAPHIC SEQUENCES IN THE MIDDLE YANGTZE & ADJACENT REGION AND EVOLUTION OF PROTOTYPE BASINS
     中扬子及邻区层序地层与原型盆地演化
短句来源
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  the middle yangtze
     PHANEROZOIC TECTONIC EVOLUTION AND ITS INFLUENCE ON THE PETROLEUM SYSTEM IN THE MIDDLE YANGTZE REGION
     中扬子地区显生宙构造演化及其对油气系统的影响
短句来源
     The Lower Ordovician reef-bearing strata in the middle Yangtze platform may be divided into four II-type depositional sequences based on the principle and method of outcrop sequence stratigraphy.
     运用露头层序地层学原理与方法,将中扬子台地早奥陶世含礁地层划分为4个II型层序,并阐述了各层序的体系域特征和形成的沉积动力学机制以及海平面变化对沉积、生物迁移、生物礁及环境的控制作用。
短句来源
     STRATIGRAPHIC SEQUENCES IN THE MIDDLE YANGTZE & ADJACENT REGION AND EVOLUTION OF PROTOTYPE BASINS
     中扬子及邻区层序地层与原型盆地演化
短句来源
     This result provided a new basis for the study of the structural features and for the prospection of mineral resources, and also provided new clues for the oil and gas exploration in the southern margin of the middle Yangtze massif.
     这一研究成果为该区构造特征研究和找矿提供了新的思路,也为中扬子地块南缘油气勘探提供了新的线索。
短句来源
     Therefore,the middle Yangtze and its adjacent region have experienced in geological history four types of prototype basins with the characteristics of episodic sedimentation.
     由此 ,中扬子及邻区在地质历史时期经历了 4种不同性质的原型盆地 ,具有幕式充填特征。
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  “中扬子”译为未确定词的双语例句
     Gravity flow sediment is well developed in lower member of Liuzuiqiao group of lower Ordivician which lies in Dashaping section of south eastern margin of Yangtze Platform.
     位于中扬子地台东南缘的大沙坪剖面下奥陶统留咀桥组下段重力流沉积非常发育,重力流沉积类型以富基质的A型碎屑流沉积为主。
短句来源
     They are bluegreen alga (containing blue bacterium and Girvanella ), Calathium, Batostoma, Pulchrilamina , and Archaeoscyphia as representation of rock sponge. They composite five types of reef-building organism community. Is bluegreen alga community (S community), Calathium bluegreen algae community (C S community), Archaeoscyphia Calathium community (A C community), Batostoma Calathium community (B C community), Batostoma Calathium bluegreen algae community (B C S community).
     中扬子台地下奥陶统红花园组造礁生物群落主要有五种 :蓝绿藻群落 (S群落 )、Calathium 蓝绿藻群落 (C S群落 )、Batostoma—Calathium群落 (B C群落 )、Archaeoscyphia—Calathium群落 (A C群落 )和Batostoma—Calathi um 蓝绿藻群落 (B C S群落 )。
短句来源
     Late Permian Eustatic Fluctuation in North Part of Central Yangtze Platform and Its Influence on Biotic Crisis Events
     中扬子北缘二叠纪晚期海平面变化对生物危机事件的影响
短句来源
     STUDY ON DOLOMITES FROM DENGYING FORMATION (SINIAN) AT THE NORTHERN MARGIN OF MIDDLE YANGTZ PLATFORM
     中扬子台地北缘灯影组白云岩研究
短句来源
     The Cambrian sequence in the Mid Yangtze area is composed of the level-high, transgressive and transitional sequences, reflecting sedimentary characteristics of a stable cratonic area.
     中扬子地区寒武系以高位型为主,其次为海侵型和过渡型,反映稳定克拉通地区沉积特征。
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  middle yangtze
new hypothesis of rice cultivation in China- middle Yangtze River and upper Huai River regions; 2.
      
The Sangzhi-Shimen synclinorium, which is in the western margin region of the Hunan-Hubei Province and as the southeast part of the middle Yangtze platform, is a second-level tectonics unit in the south of this region.
      
Three evolutionary stages of the collision orogenic deformation in the Middle Yangtze Region
      
A discussion of collision orogenic deformation has been made for the Middle Yangtze Region.
      
Middle Yangtze sea-basin over Paleozoic-Mesozoic transition
      
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  the middle yangtze
The Sangzhi-Shimen synclinorium, which is in the western margin region of the Hunan-Hubei Province and as the southeast part of the middle Yangtze platform, is a second-level tectonics unit in the south of this region.
      
Three evolutionary stages of the collision orogenic deformation in the Middle Yangtze Region
      
A discussion of collision orogenic deformation has been made for the Middle Yangtze Region.
      
Channel changes of the Makou-Tianjiazhen reach in the middle Yangtze River during the past 40 years
      
Quantitative analysis was performed on the filling-scouring process for the river reach within Makou and Tianjiazhen, the middle Yangtze River with the help of GIS and DEM techniques.
      
更多          


This paper discusses the geotectonic development in Middle Yangtse region. Three states, i. e. the development of basement (Pre-sinian), the foundation of covering strata (Sinian to Middle Triassic) and the activization (Late Triassic to Cenozoic) of platform, have been recognized. The author has divided the concerned region into the following tectonic units: the Dahongshan-Nanzhang -Fangxian depression on the margin of platform, Hansui depression, Lichuan-Jianshi depression, Qianjiang hidden uplift, Wuling...

This paper discusses the geotectonic development in Middle Yangtse region. Three states, i. e. the development of basement (Pre-sinian), the foundation of covering strata (Sinian to Middle Triassic) and the activization (Late Triassic to Cenozoic) of platform, have been recognized. The author has divided the concerned region into the following tectonic units: the Dahongshan-Nanzhang -Fangxian depression on the margin of platform, Hansui depression, Lichuan-Jianshi depression, Qianjiang hidden uplift, Wuling depression, Dayie depression, Jiangnan uplift, Shaoyang-Changsha marginal depression and Meso-Cenozoic fault-depressed basins. It is indicated that the Lichuan -Jianshi, Hansui and Wuling depressions are promising areas for searching Palaeozoic oil reservoirs; and the Cretaceous and Lower Tertiary systems in the Dongting and Boyang basins for Mesozoic and Cenozoic oil reservoirs. It is also indicated that the deep depressions in the Jianghang basin are favorable positions where the lithologic-oil-pools, concealed fault-oil-pools and bedrock-oil-pools of the Mesozoic and Cenozoic formed.

本文论述中扬子地区的地质构造演化,前震旦纪地台基底形成,震旦纪——中三叠世地台盖层形成,晚三叠世——新生代地台活化三个发展阶段。并从油气观点划分构造单元:大洪山——南漳——房县台缘坳陷;汉水坳陷;利水—建始坳陷;黔江潜伏隆起;武陵坳陷;大冶坳陷;江南隆起;邵阳——长沙边缘坳陷;中新生代断坳陷盆地。认为找古生代油藏的有利地区是:利川——建始、汉水、武陵等坳陷。找中新生代油藏是:洞庭、鄱阳盆地的白垩系及下第三系,江汉盆地深凹陷中的岩性油藏及隐蔽的断层油藏、基岩油藏等。

Li No.5 Well is situated at the eastern part of Shangzhishimeng Syn clinorium of Yangtze Platform.

澧五井位于扬了地台桑植石门复向斜东部。通过对澧五井成岩期后变化的研究和油期显示的综合分析,笔者认为:澧五井T_1d-p_1q各组的油主要来源于自层和邻近层。它们有二次生油期,第一次生油期为巴东组沉积期,此时T—P地层中有机质向石油演化还未达到最高峰,有的刚开始进入生油门限,由于印支运动二幕使地壳强烈抬升、剥蚀,地温降低,有机质停止向石油转化。第二期为燕山运动热液活动期,澧五井P—T进油期为生油期和稍后。最后指出:中扬子T—P油气的有利地区应为上覆具有较大的中新代盆地的地区。

The character of lower architexture of Middle Yangtze Area is similar to that of Upper Yangtze Area while the upper architexture is similar to that of Lower Yangtze Area. In fact, it is a polysuperposed basin consisting of an Upper Triassic - Upper Jurassic basin, a Lower and Middle Triassic - Upper Paleozoic basin, and a Sinian - Silurian basin. Generally spea-king, the petroleum richness in such a poly-superposed basin would be much higher than that in a simple basin.

中扬子区在震旦纪—志留纪期间,其总体构造格局是南接南华地槽,北邻秦岭地槽,由于南北各有一个被动大陆边缘,有利于油气的生成、运移和聚集。泥盆纪至中三叠世为一套地台型沉积,亦具有形成油气的良好地质条件。本区晚元古代至古生代的沉积、构造特点近于上扬子区,但较上扬子区活跃;而中新生代近于下扬子区,较下扬子区活动强度要弱一些。中扬子区这种“动、静相宜”的大地构造特征,为油气的生成、运移和聚集提供了良好的环境。

 
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