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阿尔塔什组
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  “阿尔塔什组”译为未确定词的双语例句
     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。
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  相似匹配句对
     ] group.
     ]
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     Group B: SD to Wistar rat heart tarnsplantation;
     B
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     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
短句来源
     ABNORMAL EVENT OF CARBON STABLE ISOTOPE AT THE BOUNDARY BETWEEN CRETACEOUS AND TERTIARY IN ALTAX SECTION IN XINJIANG AUTOAORMOUS REGION
     新疆莎车阿尔塔什剖面白垩—第三系界线的碳稳定同位素异常事件
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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。

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.

With a new understanding of petroleum geologic conditions in the Keshi Depression, southwest Tarim, the authors believe that the middle Jurassic Yangye Formation is the major source rocks in the Meso-Cenozoic systems of the area, the Kezilesu Gr. aeolian sandstones of the Lower Cretaceous could be excellent reservoirs and the overlying Upper Cretaceous and Paleogene systems are well-developed regional multiseals, among which the Artashi Fr. gypsum rocks of Palaeocene would be the best. Therefore the source rock,...

With a new understanding of petroleum geologic conditions in the Keshi Depression, southwest Tarim, the authors believe that the middle Jurassic Yangye Formation is the major source rocks in the Meso-Cenozoic systems of the area, the Kezilesu Gr. aeolian sandstones of the Lower Cretaceous could be excellent reservoirs and the overlying Upper Cretaceous and Paleogene systems are well-developed regional multiseals, among which the Artashi Fr. gypsum rocks of Palaeocene would be the best. Therefore the source rock, reservoir and regional seals may vertically and horizontally compose of an oil/gas assemblage in the depression. Based on the above considerations, a breakthrough in oil /gas exploration would be expected in proper structures.

本文通过对塔西南喀什拗陷石油地质条件的再认识,确认了中侏罗统扬叶组是本区中、新生界的主力生油岩,下白垩统克孜勒苏群中的风成砂岩为优良的储集层,覆盖其上的上白垩统和下第三系为多层系封盖性好的区域盖层,尤其是古新统阿尔塔什组石膏层更为理想的遮盖层。它们在纵横向上构成了有机的油气生储盖匹配。据此在喀什拗陷选择合适构造进行勘探,可望有新的突破。

 
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