本文關(guān)鍵詞：塔里木盆地奧陶系臺地邊緣生物礁、灘發(fā)育特征，由筆耕文化傳播整理發(fā)布。

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石油天然氣工業(yè)

地質(zhì)學(xué)

礦業(yè)工程

生物礁灘

     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.

     塔河油田中奧陶統(tǒng)一間房組廣泛發(fā)育的生物礁灘相具有臺地內(nèi)部的點(diǎn)礁、點(diǎn)灘性質(zhì),儲層的儲集空間主要是微裂縫一次生溶蝕孔隙。

短句來源

     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 .

     在層序地層格架中,生物礁灘在中期旋回 Sq11—Sq15 均有揭示,發(fā)育于海進(jìn)期旋回并在層序界面附近,礁灘發(fā)育受層控因素影響很大。

短句來源

     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.

     以柯坪小區(qū)蘇巴什剖面中發(fā)育的康克林組為例,并結(jié)合麥蓋提小區(qū)莎車縣和什拉莆剖面、阿合奇小區(qū)阿克蘇四石廠剖面,對生物礁灘體類型及特征做了深入的研究,在橫向上對康克林組或相當(dāng)于康克林組發(fā)育的礁灘體進(jìn)行了詳細(xì)的巖性、巖相對比研究,在此基礎(chǔ)上建立了研究區(qū)礁灘發(fā)育的碳酸鹽巖沉積模式。

短句來源

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

     塔里木盆地塔中地區(qū)中、上奧陶統(tǒng)生物礁灘特征及儲集體預(yù)測

短句來源

     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組沉積期生物礁灘體——以柯坪地區(qū)蘇巴什露頭剖面為例

短句來源

     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.

     中國沿海大陸架盆地油氣富集區(qū)，受下第三系富生油凹陷控制，，與其相聯(lián)系的大型披復(fù)背斜，配以大型三角洲砂巖體或大型生物礁灘灰?guī)r儲層，及大面積分布的區(qū)域蓋層，往往形成大油氣田。

短句來源

更多       

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

     對生物礁、灘的預(yù)測風(fēng)險較大；

短句來源

     The Outer Beach

     遠(yuǎn)灘

短句來源

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

     塔里木盆地奧陶系臺地邊緣生物礁、灘發(fā)育特征

短句來源

     ③Sandy Beach;

     (3)沙石灘 ;

短句來源

     DEFINITION AND CLASSIFICATION OF REEFS

     生物礁的定義和分類

短句來源

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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.

本文在概述中國氣藏的基本特征之后,列舉實(shí)例對控制氣藏形成、富集的因素進(jìn)行了分析,指出生氣中心、區(qū)域古隆起、局部古構(gòu)造、封閉型裂縫系統(tǒng)、潛伏生物礁、灘相和碳酸鹽巖的古侵蝕面等是控制我國氣藏形成、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。

陜西秦嶺泥盆紀(jì)地層中的白云巖,依據(jù)宏觀及微觀的標(biāo)志,可劃分成三大類型:同生或準(zhǔn)同生白云巖、成巖白云巖、后生白云巖。在南帶,早泥盆世的同生或準(zhǔn)同生交代白云巖,是由潮坪相的沉積物,經(jīng)咸水回流滲透白云石化作用形成,成為層控汞礦床的母巖;中泥盆世的成巖交代白云巖,是由碳酸鹽臺地相中的生物礁、灘等淺水沉積物,在大氣淡水和海水的混合水作用下白云石化而成。在北帶,泥盆紀(jì)白云巖,是由臺盆—淺海陸棚相碎屑沉積物,在埋藏壓實(shí)的條件下,經(jīng)白云石化而成。在中帶,泥盆紀(jì)白云巖主要分布于斷裂破碎帶上,是由富鎂、鈣的熱鹵水充填交代而成,并與角礫巖型的金礦(化)有密切關(guān)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.

本文應(yīng)用巖相古地理理論對南盤江地區(qū)的一些地質(zhì)構(gòu)造進(jìn)行了再認(rèn)識:由于區(qū)內(nèi)南盤江殼斷裂及百色殼斷裂的存在,引起了中三疊世巖相的劇烈變化;尼拉背斜不是一個以構(gòu)造應(yīng)力為主形成的背斜構(gòu)遣,而是一個由臺地邊緣生物礁(灘)相沉積隆起形成的兩側(cè)反傾斜的沉積構(gòu)造;對永和斷層引起的局部地段兩盤地層錯移方向與應(yīng)力分析的錯移方向相反的原因進(jìn)行了解釋。

  本文關(guān)鍵詞：塔里木盆地奧陶系臺地邊緣生物礁、灘發(fā)育特征，由筆耕文化傳播整理發(fā)布。