生物礁滩 的翻译结果

  本文关键词：塔里木盆地奥陶系台地边缘生物礁、滩发育特征，由笔耕文化传播整理发布。

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石油天然气工业

地质学

矿业工程

生物礁滩

     The organic reef and bank facies, widely developed in Middle Ordovician Yijianfang Formation in Tahe oilfield , are characterized by point reefs and banks within the caronate platforms, and the reservoir spaces are mainly of microfissures and secondary dissolution pores.

     塔河油田中奥陶统一间房组广泛发育的生物礁滩相具有台地内部的点礁、点滩性质,储层的储集空间主要是微裂缝一次生溶蚀孔隙。

短句来源

     In the chronostrigraphicframework, reef appears in third cycle:Sq11-Sq15.And reef mainly developed aroundsequence boundary in the transgression period, so the development of strata sequencecontrols the reef reservoir .

     在层序地层格架中,生物礁滩在中期旋回 Sq11—Sq15 均有揭示,发育于海进期旋回并在层序界面附近,礁滩发育受层控因素影响很大。

短句来源

     Based on the Kangkelin Formation of Subashen outcrop section in Keping country and integrated with Heshenlapu and Sishichang ones,the characteristics and types of reef-beach bodies are discussed,the lithology and lithofacies distribution are studied and the depositional model of carbonate rocks of Permo-Carboniferous in western Tarim Basin is established.

     以柯坪小区苏巴什剖面中发育的康克林组为例,并结合麦盖提小区莎车县和什拉莆剖面、阿合奇小区阿克苏四石厂剖面,对生物礁滩体类型及特征做了深入的研究,在横向上对康克林组或相当于康克林组发育的礁滩体进行了详细的岩性、岩相对比研究,在此基础上建立了研究区礁滩发育的碳酸盐岩沉积模式。

短句来源

     Distribution of the Middle-Late Ordovician reef bank reservoir in Central Tarim Basin

     塔里木盆地塔中地区中、上奥陶统生物礁滩特征及储集体预测

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     Characteristics of Reef and Beach Facies in the Kangkelin Age from Western Tarim Basin——A Case Study from the Subashi Outcrop Section in the Keping Area

     塔里木盆地西部康克林组沉积期生物礁滩体——以柯坪地区苏巴什露头剖面为例

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     Oil and gas enrichment area in basins offshore China are controlled by rich hydrocarbongenerating Paleogene depression。 Relating with large drape anticline,accompanied by largedelta sandstone reservoir or large biohermal carbonate reservoir and areal distribution of regional cap rock,large oil and gas fields could usually be formed.

     中国沿海大陆架盆地油气富集区，受下第三系富生油凹陷控制，，与其相联系的大型披复背斜，配以大型三角洲砂岩体或大型生物礁滩灰岩储层，及大面积分布的区域盖层，往往形成大油气田。

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     the predication of organic reef and bank with a higher risk;

     对生物礁、滩的预测风险较大；

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     The Outer Beach

     远滩

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     Development characteristics of organic reef-bank complex on Ordovician carbonate platform margin in Tarim Basin

     塔里木盆地奥陶系台地边缘生物礁、滩发育特征

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     ③Sandy Beach;

     (3)沙石滩 ;

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     DEFINITION AND CLASSIFICATION OF REEFS

     生物礁的定义和分类

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  organic reef

Generally, a good reservoir must be the oolite of a bank or bioclastics of an organic reef in a marginal mesa, which must deposit on the slope of the mesa.

In the region of the massif, there are good reservoirs and caprocks, many channels for gas-oil migration, and a series of structural and organic reef traps.

After summarizing the basic characteristics of gas reservoirs in (hina,this paper lists exa- mples to analyse the factors controlling the formation and aceumalation of gas reservoirs, and points out that the gas generation center,the regional palaeo-uplift,local palaeostruct- ure,sealed fracture system,hidden reef,beach facies,and the palaeo-erosion surface in carb- onate rock are all the main factors controlling the formation and ueeumalation of gas reservoirs in China.

本文在概述中国气藏的基本特征之后,列举实例对控制气藏形成、富集的因素进行了分析,指出生气中心、区域古隆起、局部古构造、封闭型裂缝系统、潜伏生物礁、滩相和碳酸盐岩的古侵蚀面等是控制我国气藏形成、富集的主要因素。

Dolomization and dolomitized rocks in Qinling,Shaanxi,are well developed.According to their macroscopic and microcosmic marks, the dolomite could be divided into three main types.They are syngenetic dolomite of para-syngenetic dolomite,diagenetic dolomite and epigenetic dolomite.In the southern belt of Qinling,syngenetic of para-syngenetic replacement dolomite of the early Devonian was formed by sediments of tidal flat facies through saline water circling and penetrating dolomiz- ation,and became the host rock...

Dolomization and dolomitized rocks in Qinling,Shaanxi,are well developed.According to their macroscopic and microcosmic marks, the dolomite could be divided into three main types.They are syngenetic dolomite of para-syngenetic dolomite,diagenetic dolomite and epigenetic dolomite.In the southern belt of Qinling,syngenetic of para-syngenetic replacement dolomite of the early Devonian was formed by sediments of tidal flat facies through saline water circling and penetrating dolomiz- ation,and became the host rock of strata-bound mercury deposit; diagenetie-replacement dolomite in the mid-upper Devonian was formed dy shallow water sediments in the carbonate platform facies through dolomization and mixed hydrations of atmospheric fresh water and sea water.In the northern belt of Qinling,the Devonian dolomite was formed by elastic sediments of platform-basin-shelf fecies through dolomization under buried and pressed conditions.In the middle belt of Qinling, the Devonian dolomite,mainly destributed in faulted shatter zones,was formed through cavity filling and metasomatism of hot-brine bearing with rich magnesium and calcium,which is closely associated with brecciated gold mineralization。

陕西秦岭泥盆纪地层中的白云岩,依据宏观及微观的标志,可划分成三大类型:同生或准同生白云岩、成岩白云岩、后生白云岩。在南带,早泥盆世的同生或准同生交代白云岩,是由潮坪相的沉积物,经咸水回流渗透白云石化作用形成,成为层控汞矿床的母岩;中泥盆世的成岩交代白云岩,是由碳酸盐台地相中的生物礁、滩等浅水沉积物,在大气淡水和海水的混合水作用下白云石化而成。在北带,泥盆纪白云岩,是由台盆—浅海陆棚相碎屑沉积物,在埋藏压实的条件下,经白云石化而成。在中带,泥盆纪白云岩主要分布于断裂破碎带上,是由富镁、钙的热卤水充填交代而成,并与角砾岩型的金矿(化)有密切关系。

This is a report on recognition of the geological structure in Nanpanjiang area.The standpoint of lithofacies and paleogeography is used in the researching process.The Nanpanjiang fault and the Baise fault exist as crust faults,they have controlled the distribution of T_2 lithofacies from the lagoon facies behind the beach to the bathal turbidity facies.The reslt is as follows:the Nila fold is not formed by structural stress,it is mainly formed by biobeach facies which formed an uplift deposit and on two sides...

This is a report on recognition of the geological structure in Nanpanjiang area.The standpoint of lithofacies and paleogeography is used in the researching process.The Nanpanjiang fault and the Baise fault exist as crust faults,they have controlled the distribution of T_2 lithofacies from the lagoon facies behind the beach to the bathal turbidity facies.The reslt is as follows:the Nila fold is not formed by structural stress,it is mainly formed by biobeach facies which formed an uplift deposit and on two sides of which the dip of deposition is opposite.This paper also explains the contradiction between the method of structural stress analysis and the method of horizon analysis about the dirction of movement of the stratum which exists in both sides of the Yonghno fault.

本文应用岩相古地理理论对南盘江地区的一些地质构造进行了再认识:由于区内南盘江壳断裂及百色壳断裂的存在,引起了中三叠世岩相的剧烈变化;尼拉背斜不是一个以构造应力为主形成的背斜构遣,而是一个由台地边缘生物礁(滩)相沉积隆起形成的两侧反倾斜的沉积构造;对永和断层引起的局部地段两盘地层错移方向与应力分析的错移方向相反的原因进行了解释。

  本文关键词：塔里木盆地奥陶系台地边缘生物礁、滩发育特征，由笔耕文化传播整理发布。