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- open-platform limestone (non-lamina dolomite mudstone microfacies)pores underdevelop with no reservoir capability. 开阔台地灰岩(非纹层纯灰泥岩微相)孔隙不发育,几乎不具备储集能力。
- evaporite platform dolomite (non-lamina dolomite mudstone microfacies) takes second place with average reservoir capability; 蒸发台地云岩(非纹层纯云泥岩微相)次之,储集性能一般;
- dolomite mudstone 白云石质泥状灰岩
- These cyclic sequences are overlain by the lagoon dolomitic mudstones and shales. 米级旋回层序之顶覆以厚度不等的?
- the most favorable microfacies belt is subordinate organisms and sparry grain dolomite microfacies, the more favorable microfacies belt is non-lamina dolomite mudstone microfacies. 最有利微相类型是生物粘结云岩微相和亮晶颗粒云岩微相,较有利的微相类型是非纹层纯云泥岩微相。
- A major topic is the origin of dolomite. 主要话题是白云岩的起源。
- Lidan, dolomite, Li Shi metres mining processing. 理石、白云石、理石米开采加工。
- It isn't limestone, it is dolomite. 这不是石灰岩，是白云岩。
- Scope: Dolomite mining. Dolomite mining. 经营范围:白云岩开采。
- Dolomite, bentonite reserves a great deal of money. 白云岩、膨润土储量也相当可观。
- Host rocks are pelitic siltstone and silty mudstone. 矿体明显受断裂控制。
- The cover rocks are marine mudstone from Pliocene to Quaternary. 储层发育有砂岩、灰岩（礁灰岩）、基岩等。
- Locally dolomite and anhydrite are important as cements. 局部地方白云石和硬石膏也是重要的胶结物。
- Sha 4 submember Kongdian Formation mudston is regional cap rock. 区域盖层为馆陶组、沙河街组四段及孔店组的泥岩层。
- We found calcite, dolomite and a few cinnabar samples there. 我们在洞内找到一些方解石、白云石及少量辰砂晶体。
- These reservoirs are mainly contained mudstone, with salts and dolomite, fracture growth, and variational reservoir lithology, which determine reservoir sensitivities are very complicated. 这种储层主要是泥岩，含盆和白云石，裂缝发育，并且岩性变化大。决定盐间非砂岩储层敏感性相当复杂。
- Cretaceous sandstone and Eogene mudstone are the main reservoir and caprock. 油气从油气田东部注入 ,由东向西运移并差异聚集 ,依次形成凝析气藏、带油环凝析气藏和挥发性油藏。
- The reservoir is usually lamina sandstone interbbeded with mudstone. 储层砂岩与泥岩大多呈薄互层状。
- The main rocks are sandstone, mudstone and muddy siltstone or silty mudstone. 岩石类型主要有砂岩、泥岩及泥-粉砂过渡岩类。
- Dolomite minerals are the characteristic part in Changjiang but few in Huanghe. 白云石在黄河中极为少见，但却是长江沉积碳酸盐中具有特色的组分。
