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Jurassic相关的网络例句

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与 Jurassic 相关的网络例句 [注:此内容来源于网络,仅供参考]

The extinction or appearance of these Ostracoda always occurred in a short time interval, and can be correlated locally and globally, so they are of importance in bioeventstratigraphy. This article listed six such biological events in Qaidam Basin and discussed their causes. The extinction of Cetacella reflected temperature decrease at global scale and changes of palaeoclimate zones during the latest Jurassic and the earliest Cretaceous; The rapid decline of Cypridea in the earliest Cretaceous may be a result of the strikes of small planets; at the latest middle-Eocene Austrocypris became extinct, and at Oligocene Hemicyprinotus disappeared. These events related to the changes of the geological conditions at that time. The explosion of Cyprideis at the middle-Miocene was because the rise of Qinghai-Xizang Plateau which resulted in the dry climate and development of salt lakes.

这些水生生物的绝灭或发生均很迅速,在区域或全球范围内均可对比,具有生物事件地层学意义:Cetacella属的绝灭可能是侏罗、白垩纪之交全球性的古气候降温和气候带变化在柴达木盆地的反映;早白垩世之后Cypridea的迅速衰退是地外因素灾变的结果;中始新世晚期的Austrocypris的绝灭、渐新世Hemicyprinotus的绝灭都与当时地质条件的改变存在著内在的联系;中中新世Cyprideis的爆发推断是青藏高原隆升,导致气候乾燥、湖水咸化的结果;而晚更新世晚期1。

The Mesozoic-Cenozoic in the Qaidam Basin contain abundant microfossils, especially in Ostracoda among which Cetacella、Cypridea、Austrocypris、Hemicyprinotus、Cyprideis and Ilyocypris inermis are index fossils for specific stratigraphical sequences since the Late Jurassic.

柴达木盆地中、新生界富含微体化石,节肢动物介形类分布尤其广泛,其中Cetacella、Cypridea、Austrocypris、Hemicyprinotus、Cyprideis和Ilyocypris inermis是晚侏罗世以来各相关层位的标准化石。

Shenglihe oil shales orientating in NWW-SEE with about 30 kilometers in length are located in the transitional belt between north Qiangtang basin and central uplift belt. The oil shales deposited in Upper Jurassic-Lower Cretaceous marine carbonates and are overlain by tremendous gypsum-salt strata.

胜利河油页岩位于北羌塘盆地与中央隆起之间的过渡带上,呈北西西-南东东向展布,长约30 km,赋矿地层为上侏罗-下白垩统海相碳酸盐岩,其上被厚层膏岩盐覆盖。

Based on the formation and separation of pan continent,the origin time of ancient species of Paeoniaceae might be back to the carboniferous of Paleozoic,and was not later than early Mesozoic.The modern species of the family flourished in Jurassic and early Cretaceous.

起源时间可以追溯到古生代的石炭纪,由于泛大陆形成与分离而形成芍药科的芍药组与北美芍药组遥相对应呈间断分布格局。

It is very difficult to get any suitable result on the basis of genus, or higher taxon in studying Jurassic bivalve palaeobiogeography.

聚类分析结果以及对控制藏北、藏南和印度侏罗纪双壳类动物群分布因素的分析表明,侏罗纪时,藏南地块的位置更靠近藏北地区,而距印度次大陆较远,与前人认识不同。

In the temproal-spatial′distribution, its source rocks is mainly Palaeogene, secondly Cretaceous and Jurassic of Mesozoic, Triassic, having mudy rocks and coal-rich, their organic carbon being 0.2% and 0.4% respectively.

提出了过渡带气综合判识标志:时空分布上,其源岩主要为下第三系,其次为中生界白垩系和朱罗系、三叠系,以泥质和煤系有机质最丰富,有机碳丰度为0.2%、后者为0.4%。

Based on the synthetic study of field outcrops, drilling section data, charts drawn in rooms, and data of stratigraphic correlation, the authors propose that the paleogeographic pattern of Ordos Basin was a fan fluvial sedimentary system at Jurassic Fuxian Stage.

在综合研究野外露头、钻井剖面及室内编图、地层对比的基础上,指出鄂尔多斯盆地冲积扇-河流沉积体系是侏罗纪富县期主要的古地理格局,富县期沉积受与古地貌密切相关的五条河谷控制。

By integrating drilling and well logging data, the Jurassic system was divided into 6 Ⅲ sequences and 17 systematical domains. The sequence boundary was identified by using the terminal correlation of seismic reflection, regional lithologic interface, changes of paleontologic distributive characters, number of logging curve and its style discontinuity. The systematical domain was divided based on the recognition of the first flooded surface and maximum flooded surface and in combination with analysis of parasequence superimposed style.

综合钻井、地震等资料,将滴南凸起侏罗系划分为6个三级层序和17个体系域,应用地震反射终止关系、区域性的岩性界面、古生物分布特征的变化、测井曲线数值和形态突变等进行了层序边界的识别;在依据岩性和测井曲线的变化识别首次湖泛面和最大湖泛面,并结合准层序叠置样式分析的基础上,进行了体系域的划分。

The basic principles of organic petrographical, organic geochemistry, sedimentology, sequence stratigraphy and the technology of micro-area and spectra analysis have been applied in the paper to study the Jurassic hydrocarbon source rock of the northern edge of Chaidamu basin. The paper reveals the features of the coal petrological, chemical composition and hydrocarbon generating mechanism of the coal bearing source rock in the studied area. It also gives the hydrocarbon generation models of different kerogen types of the area. The technology of 〓CNMR and TOFSIMS are used together to evaluate kerogen's capacity of hydrocarbon generation.

论文运用有机岩石学、有机地球化学、沉积学以及层序地层学的基本原理,综合采用多种微区及谱学分析测试技术对柴达木盆地北缘侏罗系煤系烃源岩进行了系统而深入的研究,揭示了研究区煤系烃源岩的有机组分、组成、地球化学属性以及生烃性质,建立了研究区不同类型干酪根的成烃演化模式并把〓CNMR与TOF-SIMS技术结合起来,应用于干酪根的生烃性质评价。

The characteristics of sedimentary systems and heavy minerals proved that the Junggar and Tarim Basins were not physiographically separated by an ancestral version of the Tianshan Mountains during Early-Middle Jurassic.

不同重矿物组合出现和不稳定重矿物的增加显示中-新生代存在3个构造活动相对活跃期,即晚侏罗世-早白垩世早期、晚白垩世和晚新生代。

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然而,正如其名字所指出的那样,CD盘不能写,也不能用任何方式改变其内容。

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