1)Carboniferous-Permian石炭-二叠纪
1.Deformation and metamorphic characteristics of Carboniferous-Permian coal-bearing formation and related geological hazards in Xishan (Western Hills), Beijing;北京西山石炭-二叠纪煤系变形变质特征与地质灾害
2.Analysis of Sedimentary Environment and Ascertainment of Carboniferous-Permian Lithostratigraphic Unit in South Area of Beishan, Xinjiang;新疆北山南部地区石炭-二叠纪岩石地层单位厘定及沉积环境分析
3.Geochemistry of the Carboniferous-Permian post-collisional granitic rocks from Tianshan;天山石炭-二叠纪后碰撞花岗质岩石地球化学研究
2)permo-carboniferous石炭二叠纪
1.The Cathaysia flora, which mainly flourished during the Permo-Carboniferous time in East Asia, has been held consistently in geology and palaeontology at home and abroad.主要繁盛于东亚石炭二叠纪的华夏植物群（Ｃａｔｈａｙｓｉａｆｌｏｒａ）早已驰名中外，且在地质古生物界始终有着一致认识。
2.n the basis of new viewpoint of stratigraphic correlation and by using highresolution map-making technology, a series of maps about transgressive rangs and directionshave been finished through the detailed study marine beds(limestons and marine mudstons) distributions in Permo-Carboniferous System of North China.以新的地层对比意见为基础，通过对华北石炭二叠纪海相层（石灰岩和海相泥岩）分布的详细研究，应用高分辨编目技术，完成了石炭二叠纪各期海侵范围及海侵方向图件的编制，并着重指出：①在晚石炭世早期（晋祠期）以前，郯庐断裂以西的海侵方向主体为由东向西，海侵作用中心具有由南向北迁移的规律；②自晚石炭世晚期（太原期）开始，华北盆地构造发生大的变动，古斜坡由北倾变为南倾。
英文短句/例句
1.Anthracolithic period(即石炭二叠纪) 大石炭纪
2.PERMO-CARBONIFEROUS TERRESTRIAL DEPOSITS AND PALEOGEOGRAPHIC FEATURES IN THE NORTHERN PART OF NORTHEAST CHINA东北北部石炭二叠纪陆相地层及古地理概况
3.Coal quality characteristics of carboniferous-permian coal seams of Tashan Mining Area塔山矿区石炭二叠纪煤层煤质特性研究
4.Study about Technique of Brightening of Flint Kaolin of Coal Measures in Carboniferous-Permian of Western Shandong鲁西地区石炭二叠纪煤系硬质高岭土增白技术研究
5.SEDIMENTARY TYPES AND ORGANIC CHARACTERISTICS OF HYDROCARBON SOURCE ROCKS OF CARBONIFEROUS -PERMIAN, SOUTH PART OF HUABEI南华北地区石炭二叠纪烃源岩的沉积类型与有机质特征
6.The Study of Coal Petrology and Coal Geochemistry in Permo-Carboniferous Coal from Datong Coalfield;大同煤田石炭二叠纪煤的煤岩学和煤地球化学研究
7.Sequence Stratigraphy and Coal Accumulation for Coal Measures of the Carboniferous-Permian in Hunjiang Coal Field浑江煤田石炭二叠纪含煤岩系层序地层与聚煤作用
8.Research on Sedimentary Facies of Carboniferous-Early Permian in Bachu Area;巴楚地区石炭纪—早二叠世沉积相研究
9.Characteristics and Distribution of Carboniferous-Permian Strata in Linqing Depression;临清坳陷石炭—二叠纪地层特征与分布
10.Permo-Carboniferous Coalfield Coal-Control Structure Features in Hebei Province河北省石炭—二叠纪煤田控煤构造特征
11.ON THE PERMIAN AND THE CARBONIFEROUS STRATA OF THE WESTERN HILL,TAIYUAN,SHANSI太原西山石炭纪及二叠纪地质的初步商榷
12.CHARACTERISTICS OF THE EVOLUTION AND DISTRIBUTION OF THE GLOBAL CARBONIFEROUS AND PERMIAN FLORAS全球石炭纪-二叠纪植物群的演化和分布特征
13.The Study on Carboniferous and Permian Stratigraphic Characteristics and Distribution in Jiyang Depression of Shandong;山东济阳坳陷石炭、二叠纪地层特征与分布研究
14.Permo-Carboniferous CBM Source Rock Features in Southern Hebei Area河北南部石炭—二叠纪煤层气烃源岩特征
15.Permo-Carboniferous Sequence Stratigraphy and Coal Accumulation Features in Southern Hebei河北南部地区石炭—二叠纪层序地层与聚煤特征
16.CABONIFEOUS──PERMIAN PERIOD DEPOSITION SYSTEM AND DEVELOPMENT IN THE WESTEN OF TARIM BASIN塔里木西南坳陷石炭──二叠纪沉积体系及与油气的关系
17.THE BIOSTRATIGRAPHY AND BOUNDARY BETWEEN THE CARBONIFEROUS AND PERMIAN IN SOUTHERN GUIZHOU AND NORTHWESTERN GUANGXI黔南、桂西北石炭、二叠纪之交的生物地层及其界线
18.Multiple stratigraphic division and correlation of the Permo Carboniferous of Yuzhou of Henan and Taiyuan of Shanxi河南禹州与山西太原石炭—二叠纪多重地层划分与对比
相关短句/例句
permo-carboniferous石炭二叠纪
1.The Cathaysia flora, which mainly flourished during the Permo-Carboniferous time in East Asia, has been held consistently in geology and palaeontology at home and abroad.主要繁盛于东亚石炭二叠纪的华夏植物群（Ｃａｔｈａｙｓｉａｆｌｏｒａ）早已驰名中外，且在地质古生物界始终有着一致认识。
2.n the basis of new viewpoint of stratigraphic correlation and by using highresolution map-making technology, a series of maps about transgressive rangs and directionshave been finished through the detailed study marine beds(limestons and marine mudstons) distributions in Permo-Carboniferous System of North China.以新的地层对比意见为基础，通过对华北石炭二叠纪海相层（石灰岩和海相泥岩）分布的详细研究，应用高分辨编目技术，完成了石炭二叠纪各期海侵范围及海侵方向图件的编制，并着重指出：①在晚石炭世早期（晋祠期）以前，郯庐断裂以西的海侵方向主体为由东向西，海侵作用中心具有由南向北迁移的规律；②自晚石炭世晚期（太原期）开始，华北盆地构造发生大的变动，古斜坡由北倾变为南倾。
3)Permo-Carboniferous Period石炭二叠纪
1.Igneous rock intrusion and formation mechanism in coal measures strata of Huabei Permo-Carboniferous Period;华北石炭二叠纪煤系地层火成岩侵入及形成机制
2.In order to clarify the time space distribution law of the seams of Permo-Carboniferous Period in Pingdingshan, Yuzhou and Ruzhou Mining Areas, the modern stratigraphy, sedimentology, sequence stratigraphy, and the geophysics exploration theory and method were applied to study of the comparison among the coal measures in the three coalfields.为了查明平顶山、禹州、汝州矿区石炭二叠纪煤层的时空分布规律,采用现代地层学、沉积学、层序地层学和地球物理勘探学理论和方法研究了3个煤田含煤岩系煤岩层对比。
4)Carbono-Permian coal series石炭-二叠纪煤系
1.Hydrocarbon generation and evolution of Carbono-Permian coal series from the Well Su-50 in the Wuqing Sag,Central Hebei Depression;冀中坳陷武清凹陷苏50井石炭-二叠纪煤系的成烃演化
5)Carboniferous-Permian rift石炭-二叠纪裂谷
6)Carboniferous~Pernian ice age石炭-二叠纪冰川
延伸阅读
二叠纪二叠纪（距今2.9亿年～距今2.5亿年）PermianPeriod古生代最后一个纪。这一时期形成的地层称二叠系，位于石炭系之上、中生界之下。1841年，英国地质学家R.I.莫企逊根据乌拉尔山脉西坡的彼尔姆地层，提议建立二叠系。后来发现，德国南部地层可明显地分为上、下两部分。下部为陆相红色砂岩，称赤底统；上部为海相镁质灰岩，称镁灰岩统。二叠纪地层通常分为下统和上统。也有人主张分为上、中、下统。标准地点为乌拉尔西坡的二叠系，是一套海相、半咸水相和陆相的沉积地层。下部的阿舍尔阶、萨克马尔阶和亚丁斯克阶大部为正常海相；上部的空谷阶和卡赞阶为局限的半咸水相，鞑靼阶则全为陆相。为了克服海相层位对比上的困难，有些学者引用乌拉尔以外的正常海相阶取代非海相上统的阶，自下而上为：①瓜达卢普阶。标准地点为美国得克萨斯州；②卓勒法阶。标准地点在亚美尼亚。③长兴阶。标准地点在中国浙江。二叠系二分的分界线位于瓜达卢普阶的底部；三分时，中统通常包括亚丁斯克阶和瓜达卢普阶下部的层位。海生无脊椎动物的主要门类仍是类、珊瑚、腕足类和菊石，但组成成分发生了重要变化。腕足类大为减少，仅存少数类别。类、四射珊瑚在早期繁盛，至晚期逐渐衰减而至绝灭。苔藓虫类处于衰退期。介形类的速足目渐趋繁盛。脊椎动物在二叠纪发展到了一个新阶段。鱼类中软骨鱼类和硬骨鱼类等都有发展。两栖类动物的迷齿类和爬行动物是脊椎动物的重要代表。爬行动物有3个主要分类：杯龙目、盘龙目和兽孔目。它们是现代爬行类、鸟类和哺乳动物的先祖或近亲。早二叠世的植物群与晚石炭世相似，以真蕨、节蕨、石松和种子蕨为主，晚期植物群有较大变化。鳞木类、芦木类、种子蕨、科达木等趋于衰落或濒于绝灭，而出现了银杏、苏铁、松柏类等裸子植物。二叠纪时昆虫开始迅速发展，种类大增。植物界，欧亚大陆和北美为北方植物群，下分安加拉、欧美和华夏3个植物亚群；南大陆及印度半岛为舌羊齿植物群。二叠纪的生物事件十分明显。许多门类的目或亚目在二叠纪末消亡。类在晚二叠世的40多个属，到该世结束时全部绝灭；菊石在晚二叠世的12个科，有10个科于该纪末绝灭；腕足类在晚二叠世约140个科中，到二叠末所剩极少。对这一绝灭事件虽有各种解释，但还无定论。二叠纪是地壳运动较强烈的一个纪，为华力西造山运动晚期。北美阿巴拉契亚运动是二叠纪最强烈的褶皱运动。科迪勒拉优地槽在连续的地壳运动中伴有强烈的火山活动。欧洲的造山作用和火山活动在二叠纪早期强烈，晚期趋于沉寂。早二叠世时全球性气候偏低，后期气温有所升高，北半球广布的蒸发岩沉积标志气候温暖干燥，南半球广布的含煤岩系标示为温湿气候。二叠纪有丰富的沉积矿产，主要有煤、石油和天然气、岩盐和钾盐、磷矿等。煤主要产地有西伯利亚、中国、印度、澳大利亚、北美、西欧和南非等。石油和天然气主要产于北美和东欧等地。磷矿多产于美国、乌拉尔西部、中国东南各省。
