2020
DOI: 10.1002/gj.3822
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Effects of diagenesis on natural fractures in tight oil reservoirs: A case study of the Permian Lucaogou Formation in Jimusar Sag, Junggar Basin, NW China

Abstract: Compared with conventional reservoirs, tight reservoirs experience more intense diagenesis; thus, their properties are extremely poor. Nevertheless, natural fractures with high‐strength can appear in these reservoirs and could play an essential role in the accumulation and production of tight oil. In this study, we focused on the effects of different diagenetic processes in the formation and transformation of natural fractures to determine the effects of natural fractures on tight reservoirs. Various observati… Show more

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Cited by 7 publications
(1 citation statement)
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“…e strong compaction effect makes the water flow out of the mud and also causes the microaggregation of different components of the mud, the aggregation of flake minerals and the weakly oriented laminate arrangement, forming bedding fractures; during the subperiod B and later stages of middle diagenetic rocks, transformed into dissolution, forming parallel gaps with a certain opening, which prepares space for the accumulation and storage of free gas and absorbed gas, and it is also an important type of fracture developed in the rock. e occurrence of bedding fractures is parallel or approximately parallel to the interface of the laminae, and the bedding fractures are also clearly developed in the thin shale interval with dense laminae, reflecting that the degree of development of bedding fractures in shale is closely related to the laminae [33][34][35][36]. e openings of bedding fractures usually vary greatly.…”
Section: E Impact Of Compaction On Reservoirmentioning
confidence: 99%
“…e strong compaction effect makes the water flow out of the mud and also causes the microaggregation of different components of the mud, the aggregation of flake minerals and the weakly oriented laminate arrangement, forming bedding fractures; during the subperiod B and later stages of middle diagenetic rocks, transformed into dissolution, forming parallel gaps with a certain opening, which prepares space for the accumulation and storage of free gas and absorbed gas, and it is also an important type of fracture developed in the rock. e occurrence of bedding fractures is parallel or approximately parallel to the interface of the laminae, and the bedding fractures are also clearly developed in the thin shale interval with dense laminae, reflecting that the degree of development of bedding fractures in shale is closely related to the laminae [33][34][35][36]. e openings of bedding fractures usually vary greatly.…”
Section: E Impact Of Compaction On Reservoirmentioning
confidence: 99%