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1)  carbonate turbidites
碳酸盐浊积岩
2)  carbonate sedimentary facies
碳酸盐岩沉积相
3)  carbonate rock
碳酸盐岩
1.
Inquire into Compound Oil and Gas Well Logging in Carbonate Rock of Marine Facies in Northeast Sichuan;
川东北海相碳酸盐岩油气综合录井探讨
2.
Study on the fractured reservoir of the carbonate rock in Sha 1 lower sub-interval in Wangxuzhuang Oilfield;
王徐庄油田沙一下亚段碳酸盐岩裂缝性储集层研究
3.
Research into the feasibility of the treatment of high-concentrated arsenic acidic coal mine wastewater by carbonate rocks;
碳酸盐岩处理酸性高砷煤矿废水的可行性研究
4)  Carbonate [英]['kɑ:bəneit]  [美]['kɑrbə,net]
碳酸盐岩
1.
The Characteristics and the Formation Mechanism of the Carbonate Reservoir in Jialingjiang Formation in the Southeast Area of the Southern Sichuan Basin;
蜀南东南部地区嘉陵江组碳酸盐岩储层特征及储层成因机制探讨
2.
High-precision seismic exploration in carbonate karst cave developed area;
碳酸盐岩溶洞发育区高精度地震勘探效果
3.
A study on the structural evolution and the petroleum characteristics of Gudao carbonate buried hill in Jiyang depression,China;
济阳坳陷孤岛碳酸盐岩潜山构造演化及油气成藏特征
5)  carbonate rocks
碳酸盐岩
1.
Study on diagenesis of the carbonate rocks in the Carboniferous sequence stratigraphic framework of South Guizhou;
黔南石炭系层序地层格架中碳酸盐岩成岩作用研究
2.
Restudy of tamer reservoir of buried hill of low-Paleozoic carbonate rocks in Jiyang Depression;
济阳坳陷下古生界碳酸盐岩潜山内幕储层再研究
3.
REE characteristics of carbonate rocks in Xicheng Devonian basin and origin of dolomite in Changba giant lead-zinc deposit;
西成地区碳酸盐岩REE特征及厂坝矿床白云岩成因
6)  carbonates
碳酸盐岩
1.
Seismic response and frequency difference analysis of cavern-type reservoirs in carbonates in Tahe oilfield;
塔河碳酸盐岩溶洞油藏的地震响应及频率差异分析
2.
Palaeokarst of carbonates and hydrocarbon pooling in salients surrounding Nanbao depression
南堡凹陷周边凸起地区碳酸盐岩古岩溶与油气成藏
3.
Ordovician carbonates of Tahe oilfield have been reformed by tectonic movements for many times.
塔河油田奥陶系碳酸盐岩经历了多期构造运动的改造。
补充资料:浊积岩
浊积岩
turbidite

   一种由浊流沉积作用形成的沉积岩。属半深海至深海沉积产物。按成分可分为:①钙质浊积岩。由碎屑灰岩和灰泥岩互层组成。②非钙质浊积岩。由砾岩、砂岩、粉砂岩和页岩互层组成。在纵剖面上,其特点是具鲍玛层序,即下部粗粒部分具粒序层理,其上具平行层理,再上具流水沙纹层理和包卷层理,顶部具水平纹层理,最上部为无层理的泥岩。底部常见各种印模,如槽模、沟模、锥模、重荷模等,也可见虫孔和叠瓦状构造。在碎屑石灰岩等粗粒部分含有底栖生物碎屑,在泥岩、灰泥岩等细粒部分见有浮游生物化石。一般不具有泥裂、雨痕、岩盐假象和原地植物根化石等浅水沉积物。大部分浊积岩都具有复理石建造和类复理石建造。 
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