palaeogeography中文是什么意思

• 古地理学

• "journal of palaeogeography" 中文翻译 :    古地理学报
• "palaeogeologic map" 中文翻译 :    古地质图
• "palaeogeographical" 中文翻译 :    古地理的
• "palaeogeology" 中文翻译 :    古地质学
• "palaeogeographic stage" 中文翻译 :    古地理期
• "palaeogeomorphic" 中文翻译 :    古地貌的
• "palaeogeographic reconstruction" 中文翻译 :    古地理再造
• "palaeogeomorphic map" 中文翻译 :    古地貌图
• "palaeogeographic province" 中文翻译 :    古地理区
• "palaeogeomorphic trap" 中文翻译 :    古地貌圈闭
• "palaeogeographic model" 中文翻译 :    古地理模型

• This paper is a continuation of the papers on lithofacies palaeogeography of the early , middle and late cambrian and the early and middle ordovician
  摘要本文是笔者等的中国早、中、晚寒武世和早、中奥陶世岩相古地理诸文的继续。
• The regional faults controlled the distribution of the facies , and the shaoxin - yichun fault controlles the evolution of the palaeogeography in the two sides of the fault
  在整个三叠纪，区域性大断裂对沉积相的分布具有显著的控制作用。
• Rift setting , lithofacies and palaeogeography of the basin , physical properties of the sediments , and synsedimentary faulting have played important roles in formation of the deposits
  裂谷环境、盆地的岩相古地理、沉积岩的物性特征、同沉积断裂等因素对矿床的形成起重要的控制作用。
• Liu x . m . ， t . rolph ， j . bloemendal ， j . shaw and liu t . s . ， 1995 ， quantitative estimates of palaeoprecipitation in the loess plateau of china ， palaeogeography ， palaeoclimatology ， palaeoecology ， 113 ： 243 - 248
  刘秀铭， 1997 ，中国黄土热磁研究与磁赤铁矿成因探讨，见刘嘉麒袁宝印主编‘中国第四纪地质与环境313 - 322 ，海洋出版社，北京。
• The land disappeared during the late canglangpu age and longwangmiao age ( early cambrian ) and the framework of palaeogeography consisted of tidal flat , open carbonate platform , platform - margin slopes and basin in the south
  早寒蝉寒武世中晚期岩相古地理格局由碳酸盐潮坪、开阔台地、台缘斜坡和台缘盆地组成，该地区主体进入碳酸盐台地演化阶段。
• It is the first time to discover the early paleozoic strata based on reliable fossils , which not only provides evidence to its age ascription , classification of the strata and its correlation to adjacent areas but also offers data to lithofacies , palaeogeography and tectonic pattern of studied area
  为该岩系的时代归属、地层划分及与邻区对比提供了古生物证据，也为研究该区岩相古地理、大地构造格局提供了可靠资料。
• Since the long time , different scholars had different viewpoints on stratigraphic succession ^ sedimentary environment and especially chronology evidences of the stratum , that effected infinitely the reconstruction of the tectonic evolutions and paleolithofacies palaeogeography pattern
  长期以来，不同学者对该套地层的地层层序、沉积环境、尤其是地层时代归属等均存在较大的争议，给正确恢复该区大地构造演化和岩相古地理格局带来了极大影响。
• The fluvial , delta , and lacustrine sedimentary system was realized according to the analysis of the fossils , sedimentary structure , sedimentary cycle , rhythmic bedding and other criteria in the yanchang formation . the sedimentary microfacies of the chang - 6 oil - bearing beds was identified through its fine description , and the evolution of palaeogeography was revealed
  通过古生物、沉积结构与构造、沉积韵律、沉积厚度与沉积旋回特征和测井相分析等，在延长组中识别出河流、三角洲、湖泊沉积体系，以及长6油层组的沉积微相，并对长6油层组各小层的沉积微相进行了精细描述，反演出其古地理的演化历程。
• In this paper , the author synthetically applied continental lake basin high - resolution sequence stratigraphy , sedimentation , well logging , petroleum geology , mathematics geology , etc , on the basis of studying on the core of the well drilling in the district , fully utilize logging well , well drilling core and testing and analyzing materials , adopting well logging - sedimentary facies automatical identification to study the characters of sedimentary facies and sub - facies further . and study sedimentary facies profoundly , and carry on sedimentary facies contrast well to well , to study yanchang 3 sector and yanchang 4 + 5 sector lithofacies palaeogeography character and evolution further
  本文综合应用陆相盆地高分辨率层序地层学、沉积学、测井学、石油地质学、数学地质等理论，在对研究区内有关钻井岩芯观察的基础上，充分利用测井、钻井岩芯以及测试分析资料，并采用测井?沉积相自动识别等方法，深入研究了沉积相、沉积微相特征，并进行井间沉积相对比，进而探讨了长3 、长4 + 5期的岩相古地理特征及其演化。
• Yanchang 4 + 5 sector to yanchang 3 sector lithofacies palaeogeography pattern was stable , because the constitution background was steady , and the source direction had no change , and supply was abundant . in those sectors the basin development was in lake retreat , and in the period of extinction gradually , and formatted construction delta deposit , but in yanchang 33 period the sedimentary speed were greater than construction speed , showing that overriding river mouth bars were abundant
  长4 + 5 ?长3期湖盆发展处于湖退、萎缩逐渐消亡时期，由于构造背景稳定，物源来源方向没有变化，物源供给充分，所以岩相古地理格局基本一致，形成建设性三角洲沉积，但长3 ~ 3期沉积速率大于构造沉降速率，表现为叠置河口砂坝极其发育。

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