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阿尔塔什
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     Bivalve of Paleogene at southwestern margin of Tarim Basin are divided into five assemblages which are: 1. Corbula of Aertashi Formation;
     塔里木盆地西南缘早第三纪双壳类可划分为5个组合:1.阿尔塔什组Corbula组合;
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     The source rock intervals have entered into oil window much late in the geological history, and with a higher expulsion efficiency of petroleum. The several reservoir intervals, such as O_1, C_1b, C_(1-2)k, k,C_2x and P_2, etc. , were sealed by a regional cap rocks of Aertashi Formation (E_1a) in Eogene.
     烃源岩晚期成熟,石油排运充分,阿尔塔什组区域盖层封盖,多套储集层段(Q_1、C_1b、C_(1-2)k、C_2x、P_2)等构成了麦盖提斜坡有利的石油成藏条件。
短句来源
     The results of stable carbon isotope show that obvious carbon isotope negative abnor-mality up to-3.79‰ and a fluctuation up to 6‰, have been found at the transitional time be-tween Cretaceous and Tertiary. The maximun value of negative anomaly occurs at a point of1.4m above the base of Tuilok formation.
     新疆莎车阿尔塔什剖面白垩系—第三系界线的碳同位素研究表明,在白垩系—第三系交替时期,碳同位素曾出现明显的负异常,达-3.79‰,变化幅度达6‰,负异常最大值位于原划定的吐依洛克组底界以上1.4m。
短句来源
     (5) According as Different dispatching results under different parameters combination of Aertashi reservoir, taking into account hydraulic, energy, investment index etc, the characteristic water level of Aertashi reservoir are selected by applying fuzzy optimal selection theory and grey relation analysis theory, and the optimal parameter combination is recommended.
     (5)根据阿尔塔什水库不同参数组合情况下叶尔羌河流域水库群调度结果,考虑水利、动能、投资等指标,运用模糊优选理论和灰色关联分析理论对阿尔塔什水库兴利特征水位进行了优选,推荐了最优参数组合。
短句来源
     (6) Based on deep analysis of the current study trends of reservoir operation function and various factors which affect it, the operation function of Aertashi reservoir is established by using BP neural network method and checked.
     (6)在充分分析国内外水库调度函数研究现状,以及影响水库调度函数的多变西安理工大学硕士学位论文星因子的基础上,运用改进BP神经网络方法,建立了阿尔塔什水库调度函数,并刘该函数进行了检验。
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  相似匹配句对
     A STUDY ON THE DIAGENESIS OF THE UPPER CRETACEOUS TO MIOCENE SERIES IN ARTASHI,TARIM BASIN
     新疆阿尔塔什地区上白垩统至上第三系成岩作用研究
短句来源
     GEOCHEMICAL MARKERS OF THE CRETACEOUS-IERTIARY BOUNDARY EVENT IN THE ALTAX SECTION,TARIM BASIN
     塔里木盆地阿尔塔什剖面白垩—第三系界线事件的地球化学标志
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The western part of the Tarirn Basin in Xinjiang is one of the main areas in China where marine Cretaceous and Paleocene are well developed. It is important in this region to establish Cretaceous-Paleocene strata sequences and to fix the Cre-taceous-Tertiary boundary. The marine Cretaceous is divided in ascending order into the middle-upper part of the Kezlesu Group, the Kukebai Formation, the Wuytak Formation, the Ygezya Formation, and the marine Paleocene into the Tuyr-louk Formation, the Artashi Formation...

The western part of the Tarirn Basin in Xinjiang is one of the main areas in China where marine Cretaceous and Paleocene are well developed. It is important in this region to establish Cretaceous-Paleocene strata sequences and to fix the Cre-taceous-Tertiary boundary. The marine Cretaceous is divided in ascending order into the middle-upper part of the Kezlesu Group, the Kukebai Formation, the Wuytak Formation, the Ygezya Formation, and the marine Paleocene into the Tuyr-louk Formation, the Artashi Formation and the Qimgen Formation. For about thir-ty years, the Cretaceous-Tertiary boundary had been fixed between the Tuylouk Formation and the Artashi Formation on the basis of unconformable and pseudocon-formable contact of two formations. The age of the Tuylouk Formation is the key which fix the Cretaceous-Tertiary boundary. According to some new discove-ries of foraminifera and ostracoda made during the author's field investigation, the Tuylouk Formation is assigned to the Lower Paleocene, i. e., the Danian. The fauna found in the Tuylouk Formation is quite different from that in the underlying Cretaceous Ygezya Formation which contacts conformable with the Tuylouk Formation, but bears strong resemblance to that in overlying Paleocene Qimgen Formation. Moreover, an anomalous change of carbon and oxygen isotopes occurs between the Tuylouk Formation and the Ygezya Formation. The anomalous changes in the value δ13C, δ18O and content CaCO3, as well as change in fauna are in concordance with the globe-wide catastrophic event beween the Cretaceous and Tertiary. For this reason, the Cretaceous-Tertiary boundary should be put between the Ygezya Formation and the Tuylouk Formation in this region.

塔里木盆地西部海相白垩系自下而上包括克孜勒苏群中、上部,库克拜组、乌依塔克纽和依格孜牙组,古新统包括吐依洛克组、阿尔塔什组和齐姆根组。30年来,由于证据不足,本区主要依据假整合或不整合将白垩系—第三系界线划在吐依洛克组和阿尔塔什组之间。本文根据新发现的有孔虫、介形虫等化石将吐依洛克组的时代确定为古新世早期,并根据碳氧稳定同位素、碳酸钙含量等地球化学分析,将这一界线划在依格孜牙组和吐依洛克组之间。

In this paper, the west part of the south Tianshan seismic zone and the west Kunlun seismic zone are considered as the statistic units respectively,so that parameters on seismic activity in these two units and those in potential earthquake areas being subject to them have been determined . The acceleration attenuation formula in Xinjiang region have been derived in terms of attenuation formula of seismic intensity in Xinjiang and attenuation formulas of both intensity and acceleration in the western part of...

In this paper, the west part of the south Tianshan seismic zone and the west Kunlun seismic zone are considered as the statistic units respectively,so that parameters on seismic activity in these two units and those in potential earthquake areas being subject to them have been determined . The acceleration attenuation formula in Xinjiang region have been derived in terms of attenuation formula of seismic intensity in Xinjiang and attenuation formulas of both intensity and acceleration in the western part of the United States . Finally , the exceedance probabilities of both seismic intensity and ground motion acceleration for Aratax, Kongur and Xiabandi these three engineering sites have been calculated by. an estimated method of heterogeneous time and space for seismic risk probability.

将南天山地震带西段(喀什—柯坪)和西昆仑地震带作为统计单元,确定了各单元及所属潜在震源区的地震活动性参数。利用新疆地区的地震烈度衰减公式和美国西部地区的烈度、加速度衰减公式,推算了新疆地区的加速度衰减公式。根据时空非均匀地震危险性的概率计算方法,计算了阿尔塔什、公格尔、下坂地三项工程场址的地震烈度和地动加速度超越概率。

Bivalve of Paleogene at southwestern margin of Tarim Basin are divided into five assemblages which are: 1. Corbula of Aertashi Formation; 2. Chlamys ( Ae-quipecten) tenuicostatus-Ostrea (Solidoslrea ) hemiglobosa assemblage of Qimugen Formation; 3. Ostrea (turkostrea ) turkestanensis assemblage of Kalataer Formation; 4. Fatina-Liostrea (Kokanostrea ) assemblage of Wulagen Formation; and 5 Ostrea ( Platygena ) asiatic-Amphidonta ferganensis assemblage of Bashibulake Formation. These assemblages correspond respectively...

Bivalve of Paleogene at southwestern margin of Tarim Basin are divided into five assemblages which are: 1. Corbula of Aertashi Formation; 2. Chlamys ( Ae-quipecten) tenuicostatus-Ostrea (Solidoslrea ) hemiglobosa assemblage of Qimugen Formation; 3. Ostrea (turkostrea ) turkestanensis assemblage of Kalataer Formation; 4. Fatina-Liostrea (Kokanostrea ) assemblage of Wulagen Formation; and 5 Ostrea ( Platygena ) asiatic-Amphidonta ferganensis assemblage of Bashibulake Formation. These assemblages correspond respectively with those of Bukhara Formation,SuZak Formation, Alai Formation, Turkestan Formation and Lishitan-Sumusal Formation of middle Asia in USSR.

塔里木盆地西南缘早第三纪双壳类可划分为5个组合:1.阿尔塔什组Corbula组合;2.齐姆根组Chlamys(Aequipecten)tenuicostatus-Ostrea(Solidostrea)hemig-lobosa组合;3.卡拉塔尔组Ostrea(Turkostrea)turkestanensis组合;4.乌拉根组Fatina-Liostrea(Kokanostrea)组合;5.巴什布拉克组Ostrea(Platygena)asiatica-Amphi-donta ferganensis组合.这些组合与苏联中亚布哈拉组、苏扎克组、阿赖组、土尔克斯坦组及利什坦-苏木萨尔组的组合一致.

 
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