- 更多网络例句与平地层相关的网络例句 [注：此内容来源于网络，仅供参考]
-
Deep studies on the Holocene loess-palaeosol sequences and the slack water deposits profiles, identifying and obtaining the information of paleoflood recorded in them, ensuring the amount, frequency, time and scale of the extreme Holocene paleofloods, are very helpful in revealing the characters and rules of the environment change during Holocene in this drainage basin and the middle reach of the Yellow River.
深入研究古遗址周围的黄土——古土壤地层和古洪水平流沉积物，识别和获取蕴藏其中的古洪水信息，并以此确定全新世特大古洪水事件发生的次数、频率、时间及规模，有助于揭示伊洛河流域及黄河中游地区全新世环境演变的特点和规律。
-
During drilling course,we overcome technology problems as unconsolidation formation,poor lithology,high precision of horizontal section target,thirsty formation and so on.
欢2-平1井是辽河油田第一口稀油水平井探井，油藏类型为层状边水油藏，施工过程中克服了钻经地层松散、成岩性较差、水平段中靶精度要求高、地层易漏失等技术难题。
-
On the basis of the basic principles of sequence stratigraphy,the formation of cyclical sedimentary stratum is driven by eustasy which is periodic,and by analysing the seismic,well log and nano-microfossil data of Pearl River Mouth Basin,an integrated study was conducted which is on the sequence stratigraphy of lower and middle Miocene stratum within and around Kaiping Sag .
以层序地层学基本原理——周期性海平面升降控制旋回性地层沉积——为指导，根据地震、测井和古生物资料，对珠江口盆地开平凹陷及其围区的早中新世—中中新世地层进行系统的层序地层分析，认识到该区的层序地层学特点取决于其特殊的古地理位置。
-
The study of the mineralization degree ,water type and ion combination coefficient of the Pre-Tertiary formation water in Chaluhe fault depression,Yitong Basin,reveals that total mineralization degree of the water is relatively low,and NaHCO3 water type,while the formation water has obvious vertical mineralization zonation with a high metamorphic grade.
对伊通盆地岔路河断陷古近系地层水的矿化度、水型及变质系数、脱硫系数的研究表明，该区地层水总体为NaHCO3型水；总矿化度偏低；平面上，孤店斜坡的油气保存条件最差，梁家构造带最好，垂向上，具明显的垂向分带性，万昌组保存条件最差；变质程度高。
-
During later Paleogene and early Neogene, Jiyang Depression undergone from rifting activity to depression activity. During early Guantao Formation, fault active, highland eroded, slope overlapped and sags filled, and then when later Guantao Formation begin sedimented, paleotopography became plainness, new stratum overlaid all old stratum, intensity of fault activity gradually got in weaken, and developed the sedimentary system of alluvial-fluvial-freshwater shallow lake.
济阳坳陷在古近纪晚期，新近纪早期由断陷活动转为坳陷活动，经过馆陶早期的断剥超覆和填凹补平作用，到馆陶晚期古地形渐趋平缓，新地层覆盖在所有老地层之上，断层活动强度逐渐减弱，发育冲积扇-河流-淡水极浅湖沉积体系，具有良好的生储盖配置关系。
-
According to geometry and mechanical distortion principle, a computer simulation and visualization technique is developed, which uses 2D seismic interpretative profile, tectonic plan map, sedimentary facies map and well log sheet to generate 3D tectonic-stratigraphic framework of basin, and also to establish spatial information system of real 3D digital basin.
根据几何学和机械变形原理，在具有自主知识产权的GeoView三维可视化地学信息系统平台上，研发出了通过二维地震解释剖面图、构造平面图、沉积相平面图和钻井柱状图生成真三维盆地构造－地层格架的计算机模拟和可视化技术，以及建立三维数字盆地的空间信息系统技术。
-
Paleozoic stratum can be separated east and west stratigraphical areas, according to lithological character and palaeontological information, contacted relationships and diversification of stratigraphical units in horizontal and vertical etc. The stratums in west area can be divided Devonian-Carboniferous Nanduan formation and Permian Laba formation, which is passive continental margin-bathyal depositional sequences comprised argillaceous and detrital rocks, small siliceous and carbonatite in upper. The stratums in east area can be divided lower-middle Devonian Wenquan formation and middle-upper Devonian Manxin formation, upper Devonian-lower Carboniferous Pingzhang formation, Carboniferous-Permian Yutangzhai formation, middle Permian Damingshan formation, upper Permian Shifodong formation respectively, moreover, middle-upper Permian Huoju formation is exposed in Menglian area.
根据地层的岩石组合、古生物、接触关系和地层单位的纵横向变化等特征，晚古生代的地层明显的可分为东、西两个地层小区：东部地层小区从下至上可划为泥盆—石炭系南段组、二叠系拉巴组，为一套泥质岩、碎屑岩，上部夹硅质岩、碳酸盐岩建造，属被动大陆边缘斜坡—半深海沉积；西部地层小区由下至上划分为下—中泥盆统温泉组、中—上泥盆统曼信组、上泥盆—下石炭统平掌组、石炭—二叠系鱼塘寨组、中二叠统大名山组、上二叠统石佛洞组，此外，在孟连一带尚出露中—上二叠统火居组。
- 更多网络解释与平地层相关的网络解释 [注：此内容来源于网络，仅供参考]
-
Recumbent fold：臥褶皺
偃卧褶皱(recumbent fold)为一种倒转褶皱,其轴面近乎水平,两翼平卧. 等斜褶皱(isoclinal fold)褶皱中的两翼几近互相平行,轴面的倾角或平或直或倾斜均可. 单斜层(monocline)是两端都是平缓的地层,但是中间有局部的陡急倾斜出现,
-
rootless vent：无根喷溢道
孤立地层内部褶曲;无根平轴褶曲 rootless intrafolial fold | 无根喷溢道 rootless vent | 均方根误差 root-mean-square error
-
rootless intrafolial fold：孤立地层内部褶曲;无根平轴褶曲
根牙;根齿 rooted tooth | 孤立地层内部褶曲;无根平轴褶曲 rootless intrafolial fold | 无根喷溢道 rootless vent
-
substratosphere：副平零
substrate 基质 | substratosphere 副平零 | substratum 下部地层
-
pillaret：小柱
pillardrive 地层支护平巷 | pillaret 小柱 | pillarextraction 煤柱回收
-
pillar file：平角
pillar drive ==> 地层支护平巷 | pillar file ==> 平角やすり | pillar for side panel and door ==> 侧板和门柱