2019
DOI: 10.1016/s1876-3804(19)30008-4
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Characteristics of parametamorphic rock reservoirs in Pingxi area, Qaidam Basin, NW China

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Cited by 6 publications
(4 citation statements)
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“…Based on previous studies 10 on the classification of metamorphic rock reservoir space and this study, the reservoir space of the metamorphic rock reservoir in the central paleo-uplift belt can be divided into the following four types: intergranular pores, dissolved pores, structural microfractures and weathering microfractures (Table 3 ). The main reservoir space in the chlorite schist is in the form of intergranular pores (Fig.…”
Section: Resultsmentioning
confidence: 99%
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“…Based on previous studies 10 on the classification of metamorphic rock reservoir space and this study, the reservoir space of the metamorphic rock reservoir in the central paleo-uplift belt can be divided into the following four types: intergranular pores, dissolved pores, structural microfractures and weathering microfractures (Table 3 ). The main reservoir space in the chlorite schist is in the form of intergranular pores (Fig.…”
Section: Resultsmentioning
confidence: 99%
“…It is undeniable that fractures have a very important impact on the gas production of metamorphic rock reservoirs. However, in addition to fractures, there are many pores and microfractures that are invisible to the naked eye and cannot be identified by image logging in metamorphic rock reservoirs 8 , 10 . Similar to shale, these microscopic pores and microfractures can also become reservoir spaces and flow channels for natural gas, and fracturing technology makes production of natural gas from smaller pores possible 11 .…”
Section: Introductionmentioning
confidence: 99%
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“…9-c). In the Cretaceous period, when the Huoshiling Formation was deposited, during the low-angle subduction of the Paci c Plate towards the Asia-Europe Plate, basement faults became active 44 , and the Xuxi fault began to form (Fig. 9d) 45 .…”
Section: Formation Process Of the Metamorphic Rock Reservoirmentioning
confidence: 99%