carbonate rocks 中文意思是什麼
carbonate rocks
解釋
碳酸鹽巖-
The lacustrine carbonate rocks in the wudaoliang group consist of boundstone ( stromatolite ), micritic limestone, grainstone and micritic dolostone which were laid down in the shallow - water to bathyal, high - salinity and enclosed to semi - enclosed lake systems
五道梁群湖相碳酸鹽巖分為生物粘結灰巖（疊層石） 、泥晶灰巖、顆粒灰巖與泥晶白雲巖四大類，反映出沉積環境為一個具有淺水半深水、高鹽度、半封閉封閉特點的綜合湖泊系統。 -
Carbonate rocks are predominantly composed of intra - clastic dolostone, chert dolostone and sand - bearing dolostone
碳酸鹽巖以內碎屑白雲巖、燧石白雲兒和含砂白雲巖為主。 -
This paper emphasizes the effect of the dissolution of aluminosilicate during diagenesis may provide more radiogenic strontium which would result in a high content of strontium in carbonate rocks. so we should avoid the vein of carbonate and select the samples with less terrigenous clastic, less grain content and lacking calcite cementation collected as analysis samples. the microcrystalline limestone and micro - to fine - crystalline dolomite are rather fairly whole rock samples
作者還強調了成巖過程中由長石等鋁硅酸鹽溶解提供殼源sr所造成的碳酸鹽礦物成巖蝕變可能表現為較高的sr含量；因此，在用全巖樣品進行旨在反映海水組成的各種分析時，應迴避碳酸鹽脈，選擇含陸源碎屑低、顆粒數量少、缺乏方解石膠結物的樣品，微晶灰巖或微?粉晶白雲巖是較為理想的全巖樣品。 -
The coqen basin in xizang lies between the bangong - nujiang suture zone and yarlung zangbo suture zone, and once extended northwards and southwards, respectively centred by the qiekan - goicang - asog rift zone as the center of deposition and subsidence during the middle jurassic to the early creatceous. ( 1 ) during the middle - late jurassic, the rift zone was occupied by deep - water turbidites, radiolarian siliceous rocks, shallow - water carbonate rocks, clastic rocks and basic - ultrabasic rocks, while both sides of it by littoral and shallow marine elastic rocks and carbonate rocks
摘要位於班公湖怒江縫合帶與雅魯藏布江縫合帶之間的措勤盆地，在中侏羅世早白堊世期間具有以且坎古昌阿索裂谷帶為沉積、沉降中心向南北兩側展開的古地理格局：中晚侏羅世時期，裂谷帶內由深水濁積巖、放射蟲硅質巖和淺水碳酸鹽巖、碎屑巖巖片及基性超基性巖等組成；裂谷帶兩側由濱淺海相碎屑巖和碳酸鹽巖組成。 -
The main kinds of rocks include carbonate rocks, tuffite, siliceous rocks and quartz sand - stone
主要巖石類型包括碳酸鹽巖、沈積凝灰巖、矽質巖和石英砂巖。 -
The main control factors of carbonate of preservation for information of seawater are : a ) the components of original minerals ; b ) the primary porosity of rock ; c ) the content of terrigenous elastics of carbonate rocks
有如下3個主要控制因素： a ）原始礦物組成； b ）巖石的原生孔隙度； c ）碳酸鹽巖中陸源碎屑礦物的含量。 -
The clastic rocks distribute mainly in the lower cambrian and the carbonate rocks in the upper part of the lower cambrian and middle and upper cambrian
碎屑巖主要分佈在下寒武統；下寒武統上部和中、上寒武統主要由碳酸鹽巖構成。 -
Standard test method for potential alkali reactivity of carbonate rocks as concrete aggregates rock - cylinder method
用作混凝土集料的碳酸鹽巖石潛在堿活性的標準試驗方法 -
Could there exist another possibility for the south boundary of the system as follow : the rainfall infiltrates in the outcrop carbonate - mountain area of western, and moves towards south and deeper along carbonate rocks, then moves upper through the overlain tertiary system ( n ) with a thickness of 400m ( instead of running off to the springs and yellow river through a long approach of least hydraulic gradient ), and then mainly transforms into the horizontal drainage in the loess layer of quaternary, finally drains in lu - botan depres sion
並且提出，關于對系統南界的認識，是否存在另一可能：即在西部碳酸鹽巖裸露區大氣降水入滲后，沿碳酸鹽巖向南向深部運動，然後，並非在極小的水力坡度驅動下長距離地向東部黃河、泉群徑流排泄，而是通過上覆厚度約400m的第三系向上運動，繼而主要在第四系黃土層中轉為向南水平排泄到鹵泊灘。 -
The division of diagenetic stages in carbonate rocks
碳酸鹽巖成巖階段劃分 -
In the early sinian, clastic sediments formed by fluvial and continental glacial actions were developed, while in the late sinian, great thickness of marine carbonate rocks formed by two transgression - regression cycles were developed
早震旦世發育由河流作用與陸地冰川作用形成的陸源碎屑沉積；晚震旦世則發育由兩次臺地盆地臺地的海進海退旋迴形成的巨厚海相碳酸鹽沉積。 -
Tianjin is located at north part of northern china plain, where is rich in thermal water in sedimentary basin. the main reservoir is carbonate rocks of the paleozoic and upper and middle proterozoic group, which contain thermal waters with temperature of more than 90. the cap rock is cenozoic sedimentary rocks with thickness of more than 1000m, which contains thermal water with temperature from 25 to 70 in 13 sandstone layers. the temperature of thermal water is steady growth along with the deepen of basin. all thermal waters in different aquifers are medical mineral waters, which is conducive to good health
天津位於華北平原的北部，那裡的沉積盆地含有豐富的地下熱水。主要的熱儲層為古生界和上中元古界的碳酸鹽巖層，所含熱水的溫度略高於90蓋巖層為新生界沉積層，在13個砂巖含水層中含有2570的熱水。熱水的溫度隨盆地深度的增加而增加。 -
Determination of trace elements in carbonate rocks by mnsr neutron activation analysis
微堆中子活化分析測定碳酸鹽巖中痕量元素 -
The gravity events include slumping event and turbidity - current event, and the gravity event deposits were developed in deep - water carbonate rocks in the upper sinian
重力事件可分為滑塌事件和濁流事件，其沉積產物均分佈於上震旦統，夾在大套的深水碳酸鹽巖中。 -
One of or more systems of larger openings usually occur in carbonate rocks as a result of leaching or fracturing of the primary rock material
由於原始巖石的淋濾或壓裂，導致碳酸鹽巖石中產生了一種或多種大的開孔。 -
The lacustrine carbonate rocks occur on a wide range of scales in the palaogene and neogene strata in the hoh xil basin, qinghai, and constitute an important part of the miocene wudaoliang group sediments
摘要湖相碳酸鹽巖在可可西里盆地的古、新近紀地層中分佈廣泛，更是中新統五道梁群沉積的主要組成部分。 -
Application of organic chemistrical method in discriminating oil - water strata in tarim carbonate rocks
塔里木碳酸鹽巖油水層有機地球化學判識方法 -
Through anasynthesis, sum up organic enrichment grading estimating standard of oil source rocks and gas source rocks in our country ( type ii organic matter, mature carbonate rocks )
經過分析綜合，歸納出我國碳酸鹽巖沉積區（型有機質，成熟碳酸鹽巖）氣源巖有機質豐度分級評價標準。 -
According to petrology, biological assemblage and structural features of carbonate rocks, the sedimentary environments of formations of the carbonates in yichang area are reconstructed
根據本區寒武系的巖石學特徵、生物組合特徵和沈積構造特徵重建了各組段的沈積壞境。 -
Compared to poststack time migration, prestack time migration results in clear images of fractures and cavities in the ordovician carbonate rocks, and definite unconformities at top of the ordovician
疊前時間偏移與疊后時間偏移結果相比，具有豐富的奧陶系碳酸鹽巖裂縫溶孔內幕，清晰的奧陶系頂不整合面。
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