古岩溶的英文

• palaeokarst

• "古"英文翻译    antiquity; ancientry
• "岩溶"英文翻译    karst
• "岩溶" 英文翻译 :    [地] karst◇岩溶地貌 karst landform [geomorphy]; 岩溶地形 karst topography; 岩溶湖 karst lake; 岩溶景观 karst landscape; 岩溶盆地 karstic basin; 岩溶期 karst stage; 岩溶侵蚀 karst erosion; 岩溶泉 karst source; karst spring; 岩溶水 karst water; 岩溶水文学 karstic hydrology; 岩溶现象 karst phenomenon; 岩溶作用 karstification
• "丁古岩" 英文翻译 :    tinguaite
• "古岩井" 英文翻译 :    furuiwai; koiwai
• "太古岩" 英文翻译 :    archaean rock
• "古岩性的" 英文翻译 :    palaeolithologic
• "古岩性图" 英文翻译 :    palaeolithologic map
• "古岩石分布的" 英文翻译 :    paleoareal
• "假岩溶" 英文翻译 :    pseudokarst
• "热岩溶" 英文翻译 :    thermokarst
• "岩溶带" 英文翻译 :    karst zone
• "岩溶的" 英文翻译 :    karstic
• "岩溶地" 英文翻译 :    karst region; karstregion
• "岩溶洞" 英文翻译 :    karst cave
• "岩溶沟" 英文翻译 :    grike; lapiaz; lapie
• "岩溶谷" 英文翻译 :    vale
• "岩溶河" 英文翻译 :    karst river
• "岩溶湖" 英文翻译 :    karst lake; karstic lake; sink lake
• "岩溶化" 英文翻译 :    karstification; karstify
• "岩溶井" 英文翻译 :    karst pit
• "岩溶坑" 英文翻译 :    aven
• "岩溶率" 英文翻译 :    degree of karstification
• "岩溶期" 英文翻译 :    karst stage
• "岩溶桥" 英文翻译 :    karst bridge

• The occurrence of the palaeokarstification is closely associated with the sequence boundaries and lowstand systems tract created by the guizhou - guangxi , ziyun and dongwu movements
  古岩溶作用的发生与黔桂运动、紫云运动、东吴运动等所形成的层序界面和低位体系域密切。
• One to three karst cycles may be recognized mostly at the top of the upper permian strata , top of the middle permian maokouan strata and top of the carboniferous strata and subordinately at the top of the devonian strata
  这些古岩溶作用主要存在于上二叠统顶部、中二叠统茅口组顶部和石炭系顶部，其次是泥盆系的顶部。
• The genetic types include weathering , regional meteoric corrosion , regional dolomitization regional paleokarstification , regional dedolomitization and regional fresh - water cementation and filling
  研究区存在包括风化、区域性大气淡水溶蚀、区域性白云岩化、区域性古岩溶、区域性去白云岩化和区域性淡水胶结充填等6种岩溶作用的层序成因类型。
• In this research , some conclusions are followed : l ) in the tahe oilfield , multiphase tectonic movement and pleokarst were so deeply worked on the diagenesis that the types of diagenesis are various , and the relation of those are complicated
  本次研究最终得出如下结论： 1 )研究区由于受到多期构造运动的影响，又受到多期古岩溶作用的叠加改造，成岩作用类型多样，关系复杂。
• The analysis results of hydrocarbon generating history , paleotemperature history , the homogenization temperature distribution of fluid inclusions and individual fluid inclusion compounds show that the natural gas charging times in the center gas field is two . the first is at the age of late triassic . at that time , natural gas migrated from the east to the west and from the south to the north
  根据鄂尔多斯盆地中部的沉积史、构造发育史、古岩溶形成史、生排烃史等等，按其时空配置关系，归纳气藏的形成可分为四个演化阶段：储集层孕育阶段（ 0 ； c ； ） 、圈闭形成阶段（ c 。
• Abstract : according to observation and study , the paleokarstifications of ordovician could be classified into 6 periods , i . e . depositional karstification , weathering curst karstification , burial karstification , semi - burial structural karstification , second burial karstification stage , its karstic types have mainly deposition karst , emergence karst , burial karst , wqueezing - water and structural karst or hot - water karst , and its karst - rocks can be distributed to two kinds of types , i . e . karst - sedimentary rock and karst - regenerated rock , and further to 8 subcategories and 5 sub - sub - categories in the north of anhui , china
  文摘:研究表明，皖北奥陶系古岩溶可划分为沉积岩溶作用期、风化壳岩溶作用期、埋藏岩溶作用期、构造岩溶作用期和二次埋藏岩溶作用期；其岩溶类型主要有沉积岩溶、风化壳岩溶、埋藏岩溶或压释水岩溶和构造岩溶或热水岩溶四种类型；其岩溶岩包括岩溶沉积岩和岩溶改造岩两个大类，并可进一步划分出8个亚类和5个子亚类。
• However , the authors discovered recently that the top and bottom surfaces of the loushanguan formation are palaeokarst unconformity interfaces , and there are a lot of interbeds of granular ( oolite , pisolite and oncolite ) dolomite and algae - mat dolomite , especially sedimentary structures such as the bird ? s eye , stromatolite , cross bedding and tepee structures
  但笔者新近研究发现，其顶、底均为古岩溶不整合面，并有大量颗粒(鲕、豆、核形石)白云岩和藻纹层白云岩夹层，还有许多鸟眼构造、叠层石构造、交错层理、帐蓬构造存在。
• According to observation and study , the paleokarstifications of ordovician could be classified into 6 periods , i . e . depositional karstification , weathering curst karstification , burial karstification , semi - burial structural karstification , second burial karstification stage , its karstic types have mainly deposition karst , emergence karst , burial karst , wqueezing - water and structural karst or hot - water karst , and its karst - rocks can be distributed to two kinds of types , i . e . karst - sedimentary rock and karst - regenerated rock , and further to 8 subcategories and 5 sub - sub - categories in the north of anhui , china
  研究表明，皖北奥陶系古岩溶可划分为沉积岩溶作用期、风化壳岩溶作用期、埋藏岩溶作用期、构造岩溶作用期和二次埋藏岩溶作用期；其岩溶类型主要有沉积岩溶、风化壳岩溶、埋藏岩溶或压释水岩溶和构造岩溶或热水岩溶四种类型；其岩溶岩包括岩溶沉积岩和岩溶改造岩两个大类，并可进一步划分出8个亚类和5个子亚类。
• The paper takes an example of condensed gas feild in qianmiqiao buried - hills . based on the research of formation and development of the buried - hills , three important subjects in the research are discussed with the application of advanced technical and methods ( namely , balanced cross sections , analysis of carbon isotope , mensuration of reservoir fluid inclusion ) : ( 1 ) the development of karstification and characters of reservoir in ordovician ; ( 2 ) lower tertiary ( es3 ) source in the depression nearby ; ( 3 ) the hydrocarbon generation history , migration phase and reservoir formation history
  论文以千米桥潜山凝析气藏为例，在研究潜山形成演化基础上，采用先进技术手段(平衡剖面技术、碳同位素分析、储层流体包裹体测定) ，讨论了该潜山油气藏研究中三个重要问题： ( 1 )古岩溶发育与奥陶系储层特征； ( 2 )临近凹陷下第三系油气源： ( 3 )油气生成史与运移期次以及成藏历史。