砂砾岩

砂砾岩储层预测方法研究&以东营凹陷MF地区为例

Method for Predicting Glutenite Reservoirs & Taking MF Area for Example

砂砾岩油田上倾尖灭带开发技术对策探讨

Development Technique for Updip Pinch Out Zone of Glutenite Oilfield

河南西峡琥珀产于白垩系上段（K2~3）砂砾岩中。

The samples of amber collected from the Xixia region , Henan Province , China occur in a sandy conglomerate formation of the Upper Cretaceous ( K_2 ~ 3 ) .

下部砂砾岩型矿床的成矿元素组合为CuCoPbAgAs（NiZnCd），硫同位素组成表明富集轻硫，海底热液活动不强烈；

The metallogenic element assembles in sandstone type deposits are Cu-Co-Pb-Ag-As ( Ni-Zn-Cd ), sulfur isotope is rich in light sulfur , and the contents of Ba show the thermal activity in seafloor is delicacy .

砂砾岩厚油层缓速酸酸化技术研究与应用

Application of Retarded Acid Acidizing Technology in Thick Glutenite Reservoirs

Ⅲ型，不整合面之上为砂砾岩，其下依次为泥岩、砂砾岩；

Type ⅲ glutenite above it , mudstone and glutenite below it ;

砂砾岩地层增注剂研究及应用

Development and Application of Injection Agents for Sandstone Stratum

砂砾岩地层钻头合理选型研究及应用

Study and application of bit type for glutenite formation

砂砾岩水淹层测井特点及机理研究

Logging attributes and mechanism study of grit water-flooding reservoir

砂岩、砂砾岩和基岩风化壳是油气主要储层；

Sandstone 、 conglomerate and efflorescence shell of base rock are chief reservoir zones ;

利津油田砂砾岩扇体发育特征及储层评价

Development feature of sandstone / gravel stone fan and reservoir evaluation in Lijin oilfield

砂砾岩储层有效厚度研究

Study on the effective thickness of glutenite reservoir

砾状砂岩及砂砾岩物性好，含水饱和度低。相对含油饱和度高。

While gravelly sandstones and sandy conglomerates are low water-saturated with relatively high oil saturation .

砂砾岩扇体发育特征及地震描述技术

Features and seismic description of glutenite segment

砂砾岩油藏的地球物理特征

Analysis on geophysical characteristics of glutenite reservoir

砂砾岩特稠油油藏边水综合治理技术研究及实践

The research and practice of the edge water comprehensive management technology in the glutenite super-heavy-oil reservoir

砂砾岩储层主要发育于水下冲积扇和扇三角洲中。

The sand-conglomerate reservoirs are mainly developed in both subaqueous alluvial fan and the fan delta .

砂砾岩油藏岩性、物性、电性及含油性之间的关系复杂，测井评价困难较大。

Glutenite reservoir characteristics are complicate , which is difficult to evaluate with well logging data .

砂砾岩储集层的地震反演方法

Seismic inversion for granule gravel reservoir

砂砾岩油藏高含水期控水稳油技术对策&以克拉玛依油田一区三叠系油藏为例

Technical countermeasures for water control and oil stabilization in high water-containing exploitation period of grit frame reservoir

讨论了砂砾岩型铅锌矿床的形成环境及其地质特征，概述了该类矿床的成矿时代及其空间分布规律；

This paper deals with the metallogenic environment and geological features of the sandstone-conglomerate type Pb-Zn deposits .

热储层为上第三系馆陶组和明化镇组下部砂砾岩含水层。

The thermal reservoir includes sand-gravel aquifer of Guantao Formation and the bottom of Minghuazhen Formation of Neogene .

根据图像解释的砂砾岩交错层理倾向，可推断古水流方向。

The paleocurrent direction can be deduced by dip direction of cross laminae of glutenite interpreted on images .

砂泥岩段中的砂砾岩具有单层厚度小，横向变化大的特点。

The sandstone and conglomerate in the Sand-mud-rock section have relatively small thickness of monolayer and are horizontally changeable .

通过对砂砾岩扇体的地震地质特征的总结，指出不同地区、不同时期的湖盆边缘可以形成不同类型的砂砾岩扇体；

It is pointed out that different glutenite fan might be formed on lake basin edge in different area and period .

研究成果为研究砂砾岩一类软岩的承载力提供了新的途径。

The analysis results provide new reference to the study of bearing capacity of this type in soft sandy gravel rock foundation .

碎屑岩岩石类型主要为成分成熟度及结构成熟度较低的细砾岩、砂砾岩及砾状砂岩。

The rock type of clastic reservoir are mainly conglomerate , granulated conglomerate and psephitic sandstone with low compositional maturity and low textural maturity .

通过砂砾岩厚度统计、砂砾岩百分含量分析及地震反射构型分析综合判定，研究区受北部物源控制。

The study area is controlled by the north source according to statistics of glutenite ' thickness and percentage composition , seismic reflection configuration .

砂砾岩储层的物性随着沉积环境的不同表现出较大的差异，且以扇三角洲前缘亚相水下分流河道微相最好。

Physical properties of the sandy conglomerate reservoirs differ greatly in different depositional environments , and the best occurs in underwater distributary channel on fan delta front .

砂岩和砂砾岩储集物性较好，孔隙度分布相对比较集中，各层间孔隙度虽有差异，但总体上较均质。

Sandstone and sandy conglomerate reservoir good physical properties , porosity distribution is relatively concentrated , although the difference of porosity between the layers , but in general more homogeneous .