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莱阳组
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  laiyang formation
     SEDIMENTOLOGY AND SEDIMENTARY EVOLUTION OF LOWER CRETACEOUS LAIYANG FORMATION IN JIAOLAI BASIN
     胶莱盆地下白垩统莱阳组沉积作用和沉积演化
短句来源
     The basin underwent four stages of tectonic movements: (1) Compression in NNWSSE druing the deposition of Early Cretaceous Laiyang formation;
     胶莱盆地在发展演化过程中主要经历了四期构造应力场的变化:第一期为早白垩世早期莱阳组(K1l)沉积期间,为北北西向挤压应力场;
短句来源
     The analyses of sedimentary facies, paleocurrent orientations,combined with the researches of positive tectonic units such as Dayetou uplift and Chaigou horst, indicate that Laiyang sag is a relatively independent sedimentary unit with rather deep water of deep lake or semideep lake depths controlled by Wulongcun fault during the deposition period of Laiyang formation.
     对古水流方向、大野头凸起等正向构造单元的形成时期的分析表明 :在莱阳组沉积时期 ,莱阳凹陷为一受五龙村断裂控制的相对独立的沉积单元 ,湖盆水体较深 ;
短句来源
     This paper deals with a new species of Tanychora Townes from the Upper Jurassic Laiyang Formation at Nanligezhuang village, Laiyang, Shandong.
     本文描述了我国山东莱阳莱阳组中的长室姬蜂属(Tanychora)1个新种。 这是世界上已知的最古老的姬蜂化石,在研究这个类群的起源和演化上具有重要意义。
短句来源
     Pengiakuang gold deposit was located in the denudational faults between the conglomerate of Mesozoic Laiyang Formation and the metamorphic complex of Proterozoie Jingshan Group. The orebodies were controlled by the denudational faults. The orebodies become thicker when the faults become steeper(from 15°~20°to 45°~50°).
     蓬家夼金矿赋存于中生界莱阳组和下元古界荆山群之间的剥离断层中,矿体产出严格受层间滑脱断层带控制,矿体的厚大部位产在层间滑脱断层产状由陡(45°~50°)变缓(15°~20°)处。
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  “莱阳组”译为未确定词的双语例句
     Interstratified glide breccia type gold deposit is a new type discovered from Jiaodong,occurring in interstratified glide breccia of the Jinshan Group parametamorphic rock series in Mesozoic Jiaolai Basn.
     层间滑动角砾岩型金矿是山东乳山地区新发现的金矿类型,受荆山群中的层间滑动角砾岩系控制,沿胶莱盆地边缘莱阳组砾岩与荆山群副变质岩的构造接触带分布。
短句来源
     (1) The basin was not unified and only two seperated depressions existed in the southern and the northern parts during the time of the Xiaoxianzhuang Member.
     将胶莱盆地莱阳组阮积作用的演化分为六个阶段:(1)遣仙庄段时期,该盆地尚未发育成一个统一的坳陷,只在南部和北部形成了两个凹陷.
短句来源
     Therefore, study on the icemud (sand) beds and their sedimentary structures is important and useful for climatologists and geologists to restore paleoclimate and paleogeography.
     结合黄河三角洲和莱阳盆地莱阳组马耳山段地层研究认为,对冰 泥互层及其产出的沉积构造的研究对于沉积环境和气候条件恢复具有重要意义。
短句来源
     The tectonic stress fields and the activities of strata and volcanic show that Jiaolai basin is a pull apart basin developed in Cretaceous period. The basin underwent four development steps responding to the above four stages, including initial pull apart, intermittence of pull apart, follow up pull apart and decline.
     与上述四期应力场变化相对应,由盆地中发育的地层、火山活动和构造特征可以看出,胶莱盆地是在白垩纪发育起来的一个拉分盆地,经历了4个发育阶段,即莱阳组沉积期间的初始拉分阶段、青山组沉积期间的拉分间歇阶段、王氏组沉积期间的后续拉分阶段和王氏组沉积以后的挤压隆起萎缩发育阶段。
短句来源
     The Pengjiakuang gold deposit is a new type discovered in East Shandong, which occurs in interstratified glide breccia of the Jinshan Group parametamorphic rock series in the Mesozoic Jiaolai Basin.
     蓬家夼金矿是山东乳山地区新发现的金矿类型 ,受荆山群中的构造角砾岩系控制 ,沿胶莱盆地边缘莱阳组砾岩与荆山群副变质岩的构造接触带分布。
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  相似匹配句对
     Group E is the highest.
     B
短句来源
     The SV and CO of the treatment group B increased in 5 minutes, which wa
     B
短句来源
     A NEW GENUS OF PACHYCEPHALOSAURIA FROM LAIYANG, SHANTUNG
     山东莱阳王氏中一肿头龙
短句来源
     THE DIAGENESIS OF LAIYANG FORMATION IN JIAOLAI DEPRESSION
     胶莱坳陷莱阳碎屑岩的成岩作用
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A new subfamily with a new genus and species of Platypezidae (Inse-cta,Diptera)collected from the 3rd-Member of the Early Cretaceous Laiyang Formation (K1l3)of the Laiyang Basin in the Laiyang County of Shandong province is recorded and described here together with the stratigraphic section.

本文记述山东莱阳盆地早白垩世莱阳组(K_1l_3)的扁足蝇科的1个新亚科—中国盗蝇亚科(Sinotestinae subfam.nov.).新亚科以其Sc很长,D很小,短于b_1,M_1与M_2呈叉形等等特征区别于其它两个亚科—扁足蝇亚科(Platypezinae)和小神蝇亚科(Microsaniinae);与此同时,它又兼有上述两个亚科的某些特征;在地史分布上又是早期出现的独特新类群,在分类上应有它本身的位置.文中并将含昆虫化石的地层剖面作了简要的描述.

According to sedimentary and tectonic features, this paper points out that the southern Yelrow Sea basin is a basin mainly floored by Mesozoic and Cen-ozoic terrestrial sedirnents. It consists of a scuthern and a northern depressions, the basements of which belong to Yangzi Platform and North China Platform respectively. They are very different and have to be considered respectively in planning oil and gas explorations. Oil and gas are all deriyed from source rocks. In the northern depression, the source rocks...

According to sedimentary and tectonic features, this paper points out that the southern Yelrow Sea basin is a basin mainly floored by Mesozoic and Cen-ozoic terrestrial sedirnents. It consists of a scuthern and a northern depressions, the basements of which belong to Yangzi Platform and North China Platform respectively. They are very different and have to be considered respectively in planning oil and gas explorations. Oil and gas are all deriyed from source rocks. In the northern depression, the source rocks are Wangshi Formati (previously called Taizhou Formati), Funing Formati and Laiyang Formati. The Lai-yang Formati is for the first time submitted by the authors as a possible source rock. In the southern depression, the defined source rocks are II-IV sec-tions of Funing Formati and Dainan Formati. The southern Yellow Sea basin is characterized by dustpan-shaped fault depressions, terrestrial sediments and low geothermal gradit and the effective source rocks restricted near the fault in the deep depression which controls distribution of oil and gas pools, therefore, the most favourable areas for oil finding are deep depression, fault terrace and pivotal zones. The traps with good porosity and permeabllity, which well match their formation time, and distributing within the effective source rocks are important objects for oil and gas exploration.

本文认为南黄海盆地北、南两大坳陷差异较大,部署油气勘探工作应区别对待.北坳很可能有晚侏罗世的莱阳组分布,可作为一套新的生油层.找油离不开生油中心,有效生油岩的分布控制了油气藏的分布.在这个以箕状断陷为特征的地区,以深凹带、断阶带、枢纽带为最佳油气聚集带.

This paper deals with the ostracod fossils amounting to 8 genera and 9 species(including 3 new species), which were collected from the variegated greyish-green and greyish yellow mudstone belonging to the 6th Member of the Laiyang Formation at Zhujiazhuang, 6kin north of Laiyang City in Shandong Province.The ostracod-bearing strata have been placed in the overlying Chingshan Formation based on the sequence overlapping unconformably on the metamorphic rocks of the Proterozoic Jiaodong Group by some authors.According...

This paper deals with the ostracod fossils amounting to 8 genera and 9 species(including 3 new species), which were collected from the variegated greyish-green and greyish yellow mudstone belonging to the 6th Member of the Laiyang Formation at Zhujiazhuang, 6kin north of Laiyang City in Shandong Province.The ostracod-bearing strata have been placed in the overlying Chingshan Formation based on the sequence overlapping unconformably on the metamorphic rocks of the Proterozoic Jiaodong Group by some authors.According to the writer's observation,the 6th Member of the Laiyang Formation is closely allied to the 5th Member of the same formation in lithologic characters as well as in biological aspects of conchostracans, plants, sporo-pollen, etc.,which are uniform in their stratigraphic occurrences. However, in lithologic characters the 6th Member of the Laiyang Formation is pronouncedly different from the overlying Chingshan Formation. Their contact relation is eruptive unconformity. Consequently, the strata should be referred to the Laiyang Formation.The ostracod assemblage of this member is dominated by the genus Cypridea, and may be correlated with the middle Early Cretaceous ostracods both at home and abroad. The associated remains,bivalves,plants,conchostracans,sporo-pollen, etc. with the ostracods all provide evidences supporting the conclusion of an Early Cretaceous age, and therefore the age of the ostracod-bearing strata can be suggested as of the Early Cretaceous,Descriptien of new speciesCypridea (Ulwellia)zhujiazhuangensis sp, nov.(P1. Ⅰ, figs. 5, 6)Description Carapace small-sized, elongate-elliptical in lateral view, with the greatest height at anterior one-fifth; anterior end obliquely rounded and higher than the rounded posterior end; dorsal margin straight, becoming oblique backwards from the highest position toward posterior end ventral margin straight, slightly concave medially; right valve larger than left one, overlapping. the latter ventral margin; dorsal outline elliptical, weakly convex, with the, greatest width in the postcro-median part. Hinge area slightly concave, forming a shallow sulcus; notch shallow; beak small. Surface of valves ornamented with faint punctae and tubercles which are more developed along anterior and posterior parts and arranged in a row along the dorsal margin.Measurements of this species are listed in the table (in Chinese text).Comparison This species is similar to Cypridea(Cypridea) Sp. described by Zhao Mei-yu(1985, p. 194, pt. Ⅰ, fig。 8) from the Lower Cretaceous Chingshan Formation of Mengyin, Shandong and to Cypridea (Cypridea) subconcina L. J. Zhang et Y.J. Zhang described by Zhang Li-jun et aS. (1982, p. 363, pl. 1, fig., 67) from the Lower Cretaceous Fuxin Formation of Fuxin, Liaoning, in size, lateral outline and surface ornamentation. However, it is difficult to identify whether they are uniform in species, because in the latter species, only single valves were described and illustrated, without distinguishing the overlapping relationship between two valves.Mongolianella laiyangensis sp. nov.(F1. Ⅰ, figs. 7, 8)Description Carapace large in size, elongate-elliptical in lateral view, with the greatest height at the anterior one-third; anterior end broadly rounded, higher than posterior one, which is oblique, narrowly rounded to sharply rounded, with a sharp point below and near the midline of valves; dorsal margin curved outward with no marked cardinal angles; ventral margin pronouncedly concave mediallyo.Left valve large, overlapping the right one gently along free border but strongly at the ventral margin, fusiform in dorsal view, with the greatest width behind the middle part. Surface smooth.Measurements of this species are listed in the table (in Chinese text).Comparison The new species is closely allied to Mongolianella elongata Zhang yielded from the Upper Cretaceous Daijiaping Formation of the Hengyang Basin. Hunan, but differs from the latter in the shell being smaller in size (the latter's shell reaches 2mm in length), dorsal margin weakly convex. The new

本文记述了山东莱阳县城北6km朱家庄下白垩统莱阳组第六段的介形类化石8属9种(3新种)。组合中以Cypridea属为主,已知种有Cypridea(Ulwellia)koskulensis Mandelstam, Damonella postabscissa Zhao,“Lycopterocypris”infantilis Lübimova,Candona pijiagouensis Zhang,Clinocypris scolia Mandelstam等,可与国内,外早白垩世中期的介形类动物群对比。据野外观察,莱阳组第六段与下伏层第五段的岩性相似,二者产状一致,呈过渡关系。虽然莱阳组第六段在局部地区超覆在太古界之上,但不是构造运动造成的沉积间断。而莱阳组第六段与上覆层青山组的岩性不同,二者呈喷发不整合接触。所以应将莱阳组第六段作为莱阳组的一部分,不宜划入青山组。

 
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