carboniferous

[.kɑ:bə'nifərəs]

n. 石炭纪, 石炭层
adj. 含碳或煤的, 石炭纪的

a.

含碳或煤的

carboniferous

carboniferous[,kɑ:bə'nifərəs]adj.1.■含碳的，产生碳的；含煤的

carboniferous

名词 carboniferous:

from 345 million to 280 million years ago

同义词：Carboniferous period

形容词 carboniferous:

of or relating to the Carboniferous geologic era

relating to or consisting of or yielding carbon

同义词：carbonaceous, carbonous, carbonic

carboniferous

■After 1999, the basite zone was found in the group of Kuerliang in middle-upper Carboniferous, in the Late Paleozoic strata of the North Kunlun area.

1999年以来，在北昆仑地区晚古生界中上石炭统库尔良群中发现了基性岩浆岩带。

■As one of the typical cool water brachiopod, Anidanthus had a main time range between Sakmarian of the early Permian and Wordian of the middle Permian. Several pioneers appeared in Bashkirian of the late Carboniferous.

Anidanthus是凉水型腕足动物的代表之一 ,主要出现在早二叠世Sakmarian期至中二叠世Wordian期 ,先驱分子在晚石炭世的巴什基尔期已出现 ,部分种延至晚二叠世。

■The BS basin is a Tertiary sedimentrary basin occurred on Ordovician,Silurian Carboniferous and Triassic basement strata.

BS盆地是发育在奥陶纪、志留纪、石炭纪及三叠纪基底地层之上的第三纪沉积盆地。

■Echinoconchus resembles Echinaria in the character of shells and they are important characteristic fossil of the Brachioplda in the Carboniferous.

Echinoconchus与Echinaria是特征相似同产出于石炭纪地层中的腕足动物中的两个重要标准化石属。

■Uncinunellina is a typical cold-water brachiopod and Cyathaxonia is a typical cold-water coral, which indicates that the global Carboniferous glaciation had influenced the whole area then.

Uncinunellina是典型的冷水习性腕足类,Cyathaxonia是典型的冷水习性珊瑚,表明了全球石炭纪冰期已影响到本区。

■ZHAI Yun-hong,GUO Jian-hua,LIU Sheng-guo.Study on the origine of quality clastic rocks reservoir in Carboniferous from Tazhong area[J].Journal of Mineralogy and Petrology,1996,16(2):55-61.

[1]翟永红,郭建华,刘生国.塔中地区石炭系深埋藏优质碎屑岩储层成因分析[J].矿物岩石,1996,16(2):55-61.

■DING Hui,WAN Shi-lu,LIANG Xiang-yuan.Preliminary study of Late Carboniferous conodonts biostratigraphy from Taiyuan Formation of Hebi,Henan[J].Shanxi Mining Institute Learned Journal,1983 (2):57-61.

[8]丁惠,万世禄,梁湘元.河南鹤壁晚石炭世太原组牙形石生物地层初步研究[J].山西矿业学院学报,1983 (2):57-61.

■ZHAO Xiu-qi,ZHANG Zhen-sheng,LI Hong-wen.Sequence stratigraphy and petrofacies palaeogeography of Carboniferous System in the Tarim Basin[J].Oil Geophysical Prospecting,1995,30(4):533-545.

[9]赵秀岐,张振生,李洪文.塔里木盆地石炭系层序地层学及岩相古地理研究[J].石油地球物理勘探,1995,30(4):533-545.

■A perfact Carboniferous reef complex developed on top of a volcanic seamount on the oceanic floor in the Akiyoshi Terrane, Southwest Japan.

一个完好的石炭纪生物礁发育在日本秋吉地区的玄武岩熔岩和火山碎屑岩之上。

■By the Late Carboniferous the continents that make up modern North America and Europe had collided with the southern continents of Gondwana to form the western half of Pangea.

三亿六百万年前：晚石炭纪，地质历史上强烈的成煤时期地球演化到晚石炭纪，构成今天北美和欧洲的陆块和冈瓦那南部的陆块碰撞后形成了泛大陆的西部。

■Application of ternary copolymer salt-resisting fluid loss reducer in salt bed of Carboniferous system in Tahe oilfield.

三元共聚物抗盐降失水剂在塔河油田石炭系盐层固井中的应用

■Volcanicity was violent during the Early Carboniferous in Santanghu region.The volcanic rocks consist of basalts,andesites and dacite liparite,with andesites playing the main part.

三塘湖地区早石炭世火山活动强烈，发育以安山岩类为主的玄武岩、安山岩、英安流纹岩的岩石组合。

■The biota of Upper Carboniferous is dominated by fusulinid and secondly by brachiopod and coral with flourished fossil plants in the lower pail.

上石炭统生物群以（竹蜓）类为主，腕足类、珊瑚次之，下部位物化石丰富。

■Lower Carboniferous is composed of sea facies fragments and mid-acidic component igneous rock.

下石炭统为海相碎屑岩及中酸性岩组合 ;

■The zimenqiao Formation silicolites of Lower Carboniferous is the country rock of Changkeng Au-Ag deposit.

下石炭统梓门桥组硅质岩是粤西长坑金银矿床的直接容矿岩石。

■Reservoir conditions of main reservoirs in the Fuchengzhai member,Huanglong formation,Carboniferous,and Maokou formation limestone,Permian and oolitic limestone of Dasan member,Daye formation,Tr...

且石炭系黄龙组的主要储层福成寨段、二叠系的茅口组灰岩和三叠系大冶组大三段的鲕粒灰岩储集条件均有由东向西变好的趋势。

■The Carboniferous volcanic rocks in eastern Junggar belong to basic and intermediate-acid rock assemblages and are characterized by early island-arc compression and late intraplate extension.

东准噶尔石炭系火山岩为一套基性、中酸性岩石组合，具早期岛弧挤压、晚期板内伸展环境特征。

■Metallogenic background and geochemical characteristics of Lower Carboniferous volcanic rocks in No.371-Xibeipo copper-gold mineralization belt in the Yaxi area,eastern Xinjiang.

东疆雅西371-西北坡铜金矿化带下石炭统火山岩地球化学特征与成矿背景

■In the period of Carboniferous and Early Permian, vocanic activity was strong with high geotemperature.

中三叠世时托克逊地区与科牙依地区为同一湖盆,科牙依地区为生烃中心,发育优质烃源岩;

■The research shows that the Lower Carboniferous source rock is the dominating contributor to the natur...

中下侏罗统烃源岩为一套优质烃源岩,但由于分布范围所限,贡献仅限于北缘山前带。

■In the late Carboniferous, rift bay deposit occurred in Helanshan, while widespread epicontinental sea deposit developed in the area east of paleo-mid-ridge.

中二叠世早期，研究区由北向南依次为冲积扇、辫状河、辫状河三角洲平原、辫状河三角洲前缘和滨浅湖所占据。

■Hot water sedimentation in Mesoproterozoic, action of volcanic eruption or magmatic intrusion in late Devonian and Carboniferous are main metallogenic thermal events in this region.

中元古代的热水沉积、泥盆纪的岩浆侵入和火山喷溢、石炭纪的火山作用为本区主要的成矿热事件

■The Late Carboniferous (Namurian B_C, westphalian, and stephanian) and Permian floras of China represent the Cathaysia flora.

中国的晚石炭世（纳缪尔B_C期、维斯发期和斯蒂芬期）和二叠纪植物群为华夏植物群。

■The carboniferous --permian boundary in China

中国石炭-二叠系界线

■CARBONIFEROUS MIOSPORE ZONATION IN CHINA

中国石炭系孢粉组合带序列

■Abstract The Middle Carboniferous Benxi formation in Sino-Korean paraplatform may be distinguished into two members.

中朝准地台中石炭统本溪组可分上、下两段，上段属海陆交互相夹沼泽相沉积，含不稳定的黄铁矿一层；

■As for the main reservoir-caprock assemblage , the Carboniferous volcanic rock is the reservoir while the Permian and Triassic mudstone is the cap rock.

主要的储盖组合是以石炭系火山岩为储层,二叠系和三叠系泥岩为盖层。

■Wu-Xia fault belt is a large-scale overthrust belt developed from Late Carboniferous to Triassic and faults mostly develop below the Triassic.

乌尔禾-夏子街断裂带是一个晚石炭世至三叠纪发育起来的大型逆掩断裂带,断层主要发育在三叠系以下层位,侏罗系以上近于单斜形态。

■Volcanic eruptive activities occurred from Cambrian to Permian,most intensely in Devonian and Carboniferous.

从寒武纪到二叠纪都有火山喷发，以泥盆、石炭纪火山喷发活动最强。

■The evolution of the lithofacies palaeogeography of the Carboniferous in South China was characterized with succession, development and stage.

从早石炭世岩关期至晚石炭世马平期，岩相古地理演化呈现出继承性、发展性和阶段性的特点。

■In Early Carboniferous, Tianshan mountains entered an intraplate evolution stage.

从石炭纪开始天山地区进入陆内演化阶段。

■The Carboniferous System in Hetian River Gasfield was mainly formed of a set of interbedded clastic rocks,carbonate rocks as well as interbedded gypsum,mixed plateform shore clastic and shelf facies.

以分布于和田河流域的天然柽柳灌木林地为研究对象,使用影子工程法、机会成本法等方法,评价了其生态系统服务价值。

■With sequence as drawing unit, the distribution and evolution of sedimentary facies are described and explicated in six sequences about carboniferous in the region.

以层序为作图单位，勾划并阐明本区石炭系六个层序的沉积相展布以及沉积演化规律。

■However the Late Carboniferous anomaly never completely closed, so unless the team assigned some Special Forces soldiers to guard it, more Giant Spiders could potentially come through.

但是石炭纪后期的易界口并没有完全闭合，所以除非特种部队在此驻守，否则还可能还有其它大蜘蛛穿过易界口。

■The coal-bearing rocks of the Falagou well field of Sunan County in the middle segment of the Qilianshan Mt.were composed of the Late Carboniferous shallow oceanic and continental sediments.

位于祁连山中段的肃南县法拉沟井田,含煤岩系为晚石炭世浅海型海陆交互相含煤建造。

■Hydrocarbon source rocks in North Tarim Basin can be divided into three petroleum systems such as Cambrian Ordovician system,Tertiary Jurassic system and Carboniferous Permian system.

依据塔北地区烃源岩及勘探状况 ,可划分出寒武 +奥陶系、三叠 +侏罗系及石炭 +二叠系 3套源岩含油气系统 ,其中 ,前两套为已知含油气系统 ,后者为推测含油气系统。

■Upper Jurassic red bed cover directly on coal measure strata of Permian and Carboniferous system in Yanzhou coal field .

兖州煤田的上侏罗统红层直接覆盖于二叠、石炭系煤系地层之上。

■Within the seven coal forming periods restricted to from Late Carboniferous to early Late Permian,there are seven coal groups and more than 20 seams defined in the whole area,of which seams B 3,D 2and G 7 1 are economically important.

全区自晚石炭世至晚二叠世早期所限定的7个成煤期内，共圈出煤组7个，煤层20层以上，以B3，D2，G71煤层最具工业价值。

■There is still much disagreement over the depositional characteristics of the Carboniferous Taiyuan Formation of Upper Paleozoic in the northern Ordos Basin.

关于鄂尔多斯盆地北部上古生界石炭系太原组的沉积特点,目前存在着多种不同的观点。

■During the amalgamation, the western and northern parts joined together earlierly, and formed the continent by the uplift in the early Hercynian orogeny in the late Early Carboniferous.

其中西、北两区拼合较早 ,早石炭世末的早海西运动时抬升成陆 ;

■Their formation time was not later than Early Carboniferous (C 1), and the emplacement took place before the formation of Late Triassic Yiwanshui Formation (T 3 y ).

其形成时代不晚于早石炭世（C1），侵位在晚三叠世一碗水组（T3y）之前。

■There are great bifurcations as yet on the structural environment and on the evolution of the Xingmeng Paleozoic orogenic belt in Southeast Inner Mongolia during the Carboniferous Period.

内蒙古东南部古生代造山带在石炭纪时期的构造环境和构造演化,至今在认识上存在较大的分歧。

■The volcano lava, pyroclastic rock and volcanic sedimentary rock are the main lithology of the Carboniferous volcanic reservoir in the middle section of the northwestern margin of Junggar Basin.

准噶尔盆地西北缘中段石炭系火山岩油藏的储层岩性为火山熔岩、火山碎屑岩及火山沉积岩。

■The foreland thrust belt in northwestern margin of Junggar basin is a large-scale imbricated thrust system developed since Late Carboniferous.

准噶尔盆地西北缘前陆冲断带是自石炭纪晚期发育起来的大型叠瓦冲断系统,哈拉阿拉特山冲断带为其冲断前锋构造带的东段。

■CHARACTERISTICS OF CLASTIC RESERVOIR ROCK IN CARBONIFEROUS AND PERMIAN, NORTHERN CHINA.

华北地区石炭系、二叠系碎屑岩储集层特征

■The Bogda orogen is situated between the Jungar and the Turfan Hami Precambrian blocks, and was an early to middle Carboniferous intracontinental rift, which was closed during the middle to late Carboniferous times.

博格达造山带位于准噶尔与吐鲁番 -哈密前寒武纪地块之间 ,是一个早 -中石炭世的陆内裂谷带 ,该裂谷带于中 -晚石炭世闭合。

■The deformation belts are formed by Late Carboniferous rocks, mainly mylonitization volcanic rocks and volcanic clastic sedimentary rocks.

变形带由下石炭统干墩组组成，为一套糜棱岩化火山岩、火山碎屑沉积岩。

■A number of suites of Carboniferous, middle-lower Jurassic and lower Cretaceous hydrocarbon source rocks were developed in the basin groups in the Paleo-Asian and Tethyan structural confluence area.

古亚洲与特提斯构造交汇带盆地群发育石炭系、侏罗系(中下统)、白垩系(下统)等多套烃源岩,具有厚度大、分布广、有机质丰度高的特点。

■The Palaeozoic has been broken down into six smaller units of geological time called periods. Cambrian is the oldest period of the Palaeozoic followed successively by Ordovician, Silurian, Devonian, Carboniferous and Permian Periods.

古生代可划分成6个小的叫做纪的时间单位，寒武纪是古生代中最老的一个纪，然后依次为奥陶纪、志留纪、泥盆纪、石炭纪和二叠纪。

■Arthropleura evolved from crustacean-like creatures in the Carboniferous, and grew so large because of the high percentage of oxygen in the Earth's atmosphere at that time.

古马陆从石炭纪类似甲壳类的生物中进化而来，它的体形之所以长得如此庞大，是因为当时大气层中氧的百分含量高的缘故。