diagenetic

Compression is one of the main factors that reduced the reservoir quality in early diagenetic stage.

Thereby, the change of diagenetic environments can be analyzed, and the time of pore and fissure formation can be inferred.

Textural and geochemical evidence for diagenetic interpretations are discussed, as well as techniques for interpreting diagenetic history.

The quantitative study of pore evolution shows that the pore evolution differs even at similar diagenetic stages.

The dolomitization is dominated by mixed water dolomitization in the early diagenetic stage, followed by burial dolomitization .

the main diagenetic change of feldspar is secondary growth, clay mineralization, carbonatation and dissolution.

During diagenetic process, the main factor destroying porosity is function of pressure and cementation .

Many dolomitization models have been invoked to interpret the origination of various diagenetic dolomites.

Gas layers of calcarenaceous sandstone are closely related to its diagenesis, which belong to diagenetic trap.

For diagenetic lithological hydrocarbon traps, the cutoffs of porosity or permeability and the fluid contacts control the reservoir sizes.

The main diagenetic minerals of the sandstone include calcite, chlorite, Quarta and kaolinite.

Vndergoing through the initial sedimentary stage and the diagenetic transformation stage, the present industrial ore deposit was form. . .

Stable isotopic method can be used effectively in the diagenetic research of deep water carbonate rocks.

Comprehensive analysis is made on all patterns of carbonate diagenesis and the vertical distribution features of diagenetic environments.

The ideal good ofmaize with wettability, water content is low, the bond of strong, solidification of faster, forming diagenetic.

Various " metasomatic textures" of ores were formed in diagenetic stage.

The sandstone is solidified-subsolidified, and their voids are mainly secondary voids, and the diagenetic stage is Early B.

The reasons of oil-gas richness was reasonably explained by the study on reservoir characteristic and diagenetic sequence.

In the early diagenetic stage, the development of reservoirs initiated.

Study on the diagenetic and metallogenic age of Jinchang gold deposit in Mojiang, Yunnan

The Research on Heterogeneous Reservoir by the Analysis Technique of the Diagenetic Lithofacies

Research of Sedimental Characteristics and Diagenetic Environment of Jiangbei Conglomerate

Characteristics of Diagenetic Environments of Carbonate Rocks in Western Tarim Basin and Their Controls on the Reservoir Property

the diagenetic grade, depositional microfacies, crude oil quality and well location are the main geologic factors affecting sand production;

Authigenic mineral assemblage and two types of diagenetic ambient found in the Meso-Cainozoic reservoir sandstones in Tarim basin

Isotopic Chronological Evidence for Yanshanian Diagenetic Mineralization in Baishan Rhenium-Molybdenum Mine, E. Tianshan Mountains

An quantitative assessment method of the diagenetic reservoir facies in extra-low permeability oil-gas reservoir

Strontium isotope composition of marine carbonate and the influence of diagenetic fluid on it in Ordovician

Diagenetic patterns and pore systems of the Lower Ordovician Majiagou Formation reservoirs of the central Changqing gas fields

Sequence of diagenetic authigenic mineral: the basis of timing the inclusions formation in sedimentary rocks

Diagenesis and Diagenetic Facies Studies for Yanchang Formation of the Triassic in Ordos Basin

A-type Granite of Multiple-stages and Their Diagenetic Tectonic Environment in Northeast Jiangsu Province

Diagenetic evolution of Carboniferous clastic reservoir in the southwest depression of Tarim basin

The main diagenetic change of quartz in research section is secondary growth and corrosion;

Diagenetic reservoir facies and pore space evolution of low permeability reservoir in Shaxi oilfield

Diagenetic Zone, Anchizone and Phyllosilicates in One-dimensional Nanometer Size

Research on the Diagenetic Facies of the Upper Triassic Xujiahe Formation in the Western Sichuan Foreland Basin

Single factor diagenetic facies analysis of tight reservoir in western Sichuan foreland basin

Diagenesis and division of diagenetic phases of the reservoirs in the North Weifang oil field

Diagenetic illite was separated from detrital illite and ages of diagenetic illite were obtained;

Comprehensive evaluation of diagenetic reservoir facies by gray theory

Research and application of sealing and plugging technique using GSY high-water-content swelling diagenetic agent

Reservoir Diagenetic Facies and Prediction of Oil-Beating Zones in Hudson Area of Tarim Basin

Simulation Study on Clastic Rock Diagenetic Compaction

Controlling effect of diagenetic facies on Upper Triassic tight reservoir in Moxi Gas field

Diagenetic Facies Analysis and Anomalously High Porosity Zone Prediction of the Yuanyanggou Area in the Liaohe Depression

Diagenetic-Storing Facies Division of Reservoir

Diagenetic Characters of Marine Oil-gas in Lower Yangtze Region

Diagenetic evolution and high-quality reservoir in Chang 6 sandstone in the western Ordos Basin

Research of Diagenetic Facies and Pore Evolution of Deep Low-permeabibile Reservoir in the West Slop of Qianliyuan Depression

diagenetic facies; diagenesis; Chang 8 reservoir; Zhenbei Area; Ordos Basin;

Diagenetic facies study on Chang 6-8 oil formations of Triassic Yanchang Formation in Ordos basin, China

Diagenetic mechanisms of sandstone reservoirs in China oil and gas-bearing basins