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- Lacustrine carbonate rocks in member 1 of Shahejie Formation consist of biolithitic and oolitic limestone and minor ancylus fluviatilis limestones. 摘要山东东辛油田古近系沙河街组一段湖相破酸盐岩过去仅作为盖层而忽视其油气地质意义。
- Lacustrine carbonate rocks,distributed mainly at the upper part of the 4th Memberand the middle and lower parts of the 1st Member in the Shahejie Formation,are impor-tant Eogene reservoirs in Bohai Bay Basin. 湖相碳酸盐岩是渤海湾盆地下第三系的重要油气储集层,主要分布在沙河街组四段上部和一段中、下部。
- 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. 摘要湖相碳酸盐岩在可可西里盆地的古、新近纪地层中分布广泛,更是中新统五道梁群沉积的主要组成部分。
- lacustrine carbonate rock 湖相碳酸盐岩
- EOGENE LACUSTRINE CARBONATE ROCKS AND SEDIMENTARY MODEL IN BOHAI BAY REGION 渤海湾地区下第三系湖相碳酸盐岩及沉积模式
- Alga Assembtages and Palaeoenvironment of Eogene Hetaoyuan Formation Lacustrine Carbonate Rocks in Biyang Depression, Henan Province 泌阳凹陷核桃园组湖相碳酸盐岩系藻类组合及古环境
- Petrology and sedimentary environments of the lacustrine carbonate rocks from the Miocene Wudaoliang Group in the Hoh Xil Basin,Qinghai 可可西里盆地中新统五道梁群湖相碳酸盐岩岩石学特征与沉积环境分析
- Keywords lacustrine carbonate rocks;parasequence distribution characteristics;sedimentology;sequence stratigraphy;Shahejie Formation;Huimin Sag; 湖相碳酸盐岩;准层序分布特征;沉积学;层序地层学;沙河街组;惠民凹陷;
- lacustrine carbonate rocks 湖相碳酸盐岩
- Petrology and sedimentary environments of the lacustrine carbonate rocks from the Miocene Wudaoliang Group in the Hoh Xil Basin, Qinghai (ZHOU Ken-ken, YIN Hai-sheng, LIN Jin-hui) 可可西里盆地中新统五道梁群湖相碳酸盐岩岩石学特征与沉积环境分析(周恳恳,伊海生,林金辉)
- Lacustrine carbonate will have a vast application prospect in the future future study on paleoenvironment evolution. 湖泊碳酸盐是一种研究古环境演化重要的代用指标,在过去气候环境变化研究中有广阔的应用前景。
- Hypergenesis palaeokarst contribute on carbonate rock reservoirs at most. 其中,对碳酸盐岩储层储集空间贡献最大的是表生期岩溶。
- The sedimentology and the sequence stratigraphy principles were used to study the development rules of lacustrine carbonate sedimentary cycles in the first member of Shahejie Formation. 针对惠民凹陷西部湖相碳酸盐岩储层薄、横向变化快、旋回性发育的特点,利用沉积学和层序地层学理论和方法研究了该区沙一段湖相碳酸盐岩沉积旋回的发育规律。
- The marine hydrocarbon source rock is generally carbonate rock of isolated platforms and interplatform troughs in the Baise basin. 摘要百色盆地海相烃源岩主要为孤立台地和台间海槽碳酸盐岩。
- The property of Carbonate rock on geology-geophysics and all kinds of method of hydrologic well logging were analyzed. 本文分析了碳酸盐岩地层的地质-地球物理特征和各类测井方法对它的响应。
- A complete laterite profile should be made up of laterite layer, parti-color clay layer and carbonate rock saprolite. 完整的红土剖面应该由红土层、杂色粘土层和碳酸盐岩腐岩组成。
- lacustrine carbonate source rocks 湖相碳酸盐岩
- The sedimentary facies relating with carbonate rock include lakeshore, bank, bank margin, bathyal lake subfacies. 生物浅滩具有分布范围广阔、顶面平坦、进积迅速、前斜坡明显、沉积旋回发育、沉积厚度较小但稳定的特征。
- Carbonate rock saprolite is formed in zones of alteration and made up of travertine and residual carbonate crystals. 碳酸盐岩腐岩形成于包气带,由原岩中的碳酸盐溶解后再次沉淀形成,主要由钙华和残馀碳酸盐晶体组成。
- There are some fluid inclusions in the fillings of dissolved void of Ordovician carbonate rock in the Ordos basin. 鄂尔多斯盆地奥陶系马家沟组碳酸盐岩的溶孔、溶洞充填物中均含有一定量的包裹体。