carbonatite 中文意思是什麼
carbonatite
解釋
碳酸鹽巖-
The determinative characteristics of common rock forming minerals containing quartz group, feldspar group, mica group, hornblende group, pyroxene group, olivine group and carbonatite minerals will be discussed in greater detail
對常見造巖礦物，如石英類、長石類、雲母類、角閃石類、輝石類、橄欖石類、碳酸鹽類礦物的鑒定特徵將予以詳細的說明。 -
The paper adopts some methods such as gas composition, carbon isotope, systematical analyzing and testing of reservoir bitumen biomarker from high evolutional natural gas and quantitative calculation of mixed gas, illustrates that natural gas from the section of jialingjiang formation is mainly attributed to sapropel type organic matter gas of permian, comes from carbonatite hydrocarbon rocks permian which most of them are overmature, its main gas source has nothing to do with carbonatite hydrocarbon rocks of jialingjiang formation themselves, presents in geochemistry characteristics of oil type cracked gas
摘要通過對川中川南過渡帶西部的磨溪潼南地區嘉二段天然氣組成、碳同位素組成、高演化天然氣儲層瀝青生物標志化合物的系統分析測試和混合成因氣的定量估算，闡明了該區嘉二段天然氣主要屬於二疊系腐泥型有機質成因氣，來源於二疊系過成熟為主的碳酸鹽巖烴源，主力氣源與嘉陵江組自身的碳酸鹽巖烴源無關，並具有油型裂解氣的地球化學特徵。 -
Reefs are well developed in western hubei and eastern chongqing. through sedulous research, the whole acquaintance on types of reef builders, types of reef carbonatite, development and evolution of reef organisms, division of reef facies, distributing regularities of reefs and diagenesis has been concluded. according to the comprehensive studies, the following results and conclusions have been obtained
通過對鄂西渝東區上二疊統長興組生物礁造礁生物、沉積相、成巖作用的研究，認清了礁體的主要造礁生物類型、主要巖石類型、生長演化、相帶劃分、分佈規律以及成巖作用，可以得出以下結論和認識： 1生物礁主要分佈於晚二疊世碳酸鹽臺地內部和臺地邊緣，可分為三種類型。 -
Thermolysis production of lake carbonatite organic matter and its carbon isotopic composition characteristic
湖相碳酸鹽巖有機質熱演化產物及其碳同位素組成特徵 -
Research on retarder available for alkali activated carbonatite - slag cementitious material
礦渣膠凝材料的緩凝劑研究 -
Carbon and oxygen isotope data show that the carbonatite layer in fozichong ledge is different from the normal marine sedimentary carbonatite, infering that its formation has relation with hot - water sedimentary activity
碳、氧同位素顯示，佛子沖礦田賦礦層位中的碳酸鹽巖地層與正常的海相沉積碳酸鹽巖不同，其成因與熱水沉積活動有關。 -
In the thesis, the ree concentration and ree distribution patterns are also studied for stream water, granite fissure water and water from carbonatite around the baisha region
本文還討論了該區的河水、花崗巖裂隙水、灰巖出露地區地下水的稀土含量及其分佈模式。 -
Lithology should be determined by comprehensive analysis and judgment through chemical agents analysis method and microscope amplification description combined with outlook characteristics description, integrated with regional data and comprehensive logging data in the course of cutting logging in southern marine carbonatite
摘要南方海相碳酸巖巖屑錄井應以化學試劑分析法、顯微鏡放大描述法為主，輔以外觀特徵描述法，結合區域資料、綜合錄井資料、綜合分析、判斷，確定巖性。 -
Influence of ultra - low water saturation on condensate carbonatite reservoir develepment
碳酸鹽巖凝析油氣藏超低含水飽和度及其對開發動態的影響 -
It is very resembly representative island arc volcanic rock in the geochemistry character, so i demonstrate that a petrofabric formed tectonic activity section and island arc environment ; i also demonstrate that parametamorphite in the a petrofabric formed tectonic activity section. b petrofabric is very resembly a petrofabric in many aspects, so i think that b petrofabric also formed island arc environment, but volcanic activity obvious weakened in the b petrofabric stage. c petrofabric formed carbonatite mesa
在地球化學特徵方面與典型島弧火山巖非常相似，得出a巖組形成於構造活動區，形成環境為島弧環境。 a巖組的副變質巖的原巖碎屑巖是快速堆積的，處于構造活動區。 b巖組和a巖組對應的巖石在各個方面都非常相似，所以形成環境也為島弧環境，只是火山活動在這期間明顯減弱。 -
Huge deep fractures in the east of china have a little influence on the pore of carbonatite reservoir of ? - o stratum in the regions of zhuangxi and chengdao. the karstification which probably happened at xishan tectogenesis period is also very limited
我國東部深大斷裂對樁西、埋島地區寒武一奧陶系碳酸鹽巖的儲層孔隙影響很小，可能發生在喜山期的巖溶作用（深部流體帶來的巖溶作用）也是十分有限的。 -
The result demonstrates the method of seismic attribute is an effective tool to study carbonatite reservoir
研究表明地震屬性技術是研究碳酸鹽巖的有效工具。 -
The basic principle of forward modeling technique shows that it is essential to do forward modeling well when predicating carbonatite reservoir
摘要模型正演的基本原理表明，在碳酸鹽巖儲層預測時做好模型正演工作是十分必要的。 -
On the basis of these studies, the method of seismic attribute is applied to the exploration of carbonatite in buried hill in in sangtamu area, talimu basin
在對地震屬性理論研究的基礎上，將其應用於塔里木盆地桑塔木地區潛山構造的碳酸鹽巖儲層的研究。 -
Closely connecting the theory of seismic attribute with its application, we study the method to fit to the exploration of carbonatite reservoir in sangtamu area
將地震屬性的理論研究與實際應用緊密結合，探索出適合桑塔木地區油氣勘探的地震屬性研究方法。 -
The bareness carbonatite rock in chongqing is about 3. 91 x 104km2, makes up of 50 % of the overall land, and distributes mostly at northeast ( include three gorges reservoir area ) and southeast counties of chongqing
重慶市碳酸鹽巖出露面積約3 . 91萬km ~ 2 ，約占幅員總面積（ 8 . 24萬km ~ 2 ）的50 ，主要集中分佈於渝東北（其中包括三峽庫區）和渝東南各區市縣。
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