geologic background中文是什么意思

• 地质背景

• "geologic"中文翻译    adj. 地质学的，地质的。 a geologic su ...
• "background"中文翻译    n. 1.后景，背景；基本情况；(纺织品等的)底子；出身 ...
• "geologic" 中文翻译 :    adj. 地质学的，地质的。 a geologic survey 地质调查。 adv. -ically
• "background" 中文翻译 :    n. 1.后景，背景；基本情况；(纺织品等的)底子；出身；经历。 2.隐蔽的[不引人注目的]地位；幕后。 3.衬托音乐，伴音；【无线电】干扰杂音 (students of workers' background. 工人出身的学生)。 in the background 背地下，背后；在幕后(活动)。
• "in the background" 中文翻译 :    在背后, 在幕后, 作为后果
• "geologic fracture, geologic rift" 中文翻译 :    地质断裂
• "geologic =geological" 中文翻译 :    地质的
• "geologic abundance" 中文翻译 :    地质丰度
• "geologic action" 中文翻译 :    地质作用
• "geologic age" 中文翻译 :    地质代; 地质年代; 地质期; 地质时代
• "geologic agent" 中文翻译 :    地质因素
• "geologic ages" 中文翻译 :    地质年代
• "geologic airview" 中文翻译 :    航空地质目测
• "geologic analogue" 中文翻译 :    地质类比法
• "geologic analysis" 中文翻译 :    地质分析
• "geologic anomaly" 中文翻译 :    地质变态; 地质异常
• "geologic application" 中文翻译 :    地质应用
• "geologic aspects" 中文翻译 :    地质概况
• "geologic barometer" 中文翻译 :    地质压力计
• "geologic basin" 中文翻译 :    地质盆地
• "geologic body" 中文翻译 :    地质体
• "geologic boundary" 中文翻译 :    地质界线
• "geologic characteristic" 中文翻译 :    地质特征
• "geologic chemistry" 中文翻译 :    地质化学
• "geologic chronology" 中文翻译 :    地质编年学。

• Starting from the study of geologic background of carboniferous - permian organic mass thermal evolution in south huabei area , a study is conducted on the genesis of thermal evolution of organic mass
  摘要从南华北地区石炭系二叠系有机质热演化的区域地质背景研究入手，根据其有机质热演化程度及其分布规律，对有机质热演化的成因类型进行了研究。
• At present , research on low resistivity oil zone has been deepened in microscopic mechanism , but the research for intrinsic relation between the zone and geologic background factors is incomplete and lack of productive forecast and directivity
  摘要目前低电阻率油气层研究面临的问题是微观机理分析较深入，地质背景因素与低电阻率油气层的内在联系探讨不多，缺乏对生产的预测性和指导性。
• Geologic background factors play an important controlling role in geneses of the zone with different characteristics in stress field , distribution of sedimentary facies or source condition , etc . , all these , more or less , influence or control the final geneses of such a zone
  论述了地质背景因素对低电阻率油气层的形成具有重要的控制作用，在盆地的演化过程中应力机制、沉积相展布及物源等方面表现出的不同性，都或多或少地影响或控制了低电阻率油层的最终成因。
• 2 . tazhong ancient uplift originated from normal fault in paleozoic , hydrocarbon formed in ordovician period , structure reverse made tazhong uplift form from the middle ordovician period to the late ordovician period , and it provided geologic background for the deposit of silurian - devonian stratum . tazhong uplift formed at the end devonian , ancient reservoir was destroyed and asphaltum sandstone formed , structure deformation more destroyed ancient reservoir in early permian , after then the major of structure deformation is regulation
  塔中隆起源于早古生代拉张背景下的正断层，寒武-奥陶纪为其烃源岩形成的重要时期；早奥陶世末-晚奥陶世末的构造反转是塔中隆起的主要形成期，同时也为志留系形成地层及复合圈闭提供了古地理背景；志留?泥盆纪塔里木盆地南北缘均转为活动大陆边缘，形成了大量的断裂和不整合；泥盆纪末塔中鼻状隆起基本定型，古油藏遭受破坏，形成了沥青砂岩；早二叠世晚期的构造变形使古油藏遭受进一步的破坏；二叠纪后构造变动主要以调节为主。
• In this paper , the author deals with the metallogenic characteristics and forecast of gold deposits in fujian province . on the basis of the geologic scientific achievements yielded by forefathers , the author discusses the geologic background of fujian province in great detail , which provides the basic data for studying the ore control factors , the metallogenic law and the forecast of gold deposits
  在认真收集和消化吸收前人资料的基础上，研究和分析了福建省金矿产出的区域地质背景和构造岩浆演化特征，并对福建省区域地球物理和地球化学特征进行了总结，为研究金矿的控矿地质条件、成矿规律和成矿预测提供了翔实的基础资料。
• The genesis of spots in ore - bearing rock of baguamao gold deposit has been elaborated , through the geologic background , the characteristics of ore - bearing bed , the mutiperiodic mineralization and the mineral composition . the author indicates that the mottled structure of devonian system in qinling mts . resulted from the mutiperiodic activity of ore fluid and connected with the gold mineralization ， in addition ， it could be regarded as one of the important marks for gold mineralization
  主要从成矿地质背景，含矿层特征和多期成矿等方面阐述了八卦庙金矿含矿岩石中斑点的物质组成及其特征，指出秦岭泥盆纪含矿岩石中斑点状构造为成矿流体多期作用的结果且与金矿化关系密切，可作为金矿化的重要标志之一。
• In this paper , based on former researching works and regional geologic background analysis , we studied the distribution law of copper and geotectonic metallogenic characteristics of the ore deposit , and forecasted copper enrichment trend from copper deposit geologic characteristics " view , aiming at full understanding the metallogenic characteristics of dongxiang copper deposit
  本文针对东乡铜矿成矿特点，结合前人工作成果，在对区域地质背景分析的基础上，从铜矿地质特征着手，对铜元素分布规律、铜矿构造成矿特征及富矿预测进行深入剖析。
• At first , the writer particularly introduces the theoretical frame of the development of ecotourism in sichuan wang lang nature reserve after summarizing simple content of nature reserve and ecotourism . following , the author has narrated the environmental condition such as geologic background and landform characteristics and has a eco - tourism proposition
  论文首先对自然保护区与生态旅游进行了简单概述，然后叙述了王朗自然保护区的地质背景、地形地貌等生态旅游开发的环境条件，详细介绍了王朗自然保护区的生态旅游开发条件，并作了生态旅游发展构想。
• Abstract : analysing the geologic background of interlayer oxidation zone in the north of junggar basin from the aspects of basin structure , the structural feature and lithofacies and lithologic conditions of the sedimentary cover , as well as the regional hydrogeology and reducing medium of the sedimentary cover , this paper suggests that the study area possesses abundant uranium source and the stratigraphic combination favourable for the development of interlayer oxidation zone
  文摘:本文从盆地结构、沉积盖层的构造特征、岩相岩性条件、区域水文地质条件、还原介质条件等方面分析了准噶尔盆地北部层间氧化带形成的地质背景，认为该区具有丰富的铀源条件及适合层间氧化带发育的地层组合。
• Abstract : the genesis of spots in ore - bearing rock of baguamao gold deposit has been elaborated , through the geologic background , the characteristics of ore - bearing bed , the mutiperiodic mineralization and the mineral composition . the author indicates that the mottled structure of devonian system in qinling mts . resulted from the mutiperiodic activity of ore fluid and connected with the gold mineralization ， in addition ， it could be regarded as one of the important marks for gold mineralization
  文摘:主要从成矿地质背景，含矿层特征和多期成矿等方面阐述了八卦庙金矿含矿岩石中斑点的物质组成及其特征，指出秦岭泥盆纪含矿岩石中斑点状构造为成矿流体多期作用的结果且与金矿化关系密切，可作为金矿化的重要标志之一。