Title Fractal behaviors of NMR saturated and centrifugal T-2 spectra in oil shale reservoirs: The Paleogene Funing formation in Subei basin, China
Authors Liu, Xiaoping
Jin, Zhijun
Lai, Jin
Fan, Xuechun
Guan, Ming
Shu, Honglin
Wang, Gaocheng
Liu, Mengcai
Luo, Yufeng
Affiliation China Univ Petr, State Key Lab Petr Resources & Prospecting, Beijing 102249, Peoples R China
China Univ Petr, Coll Geosci, Beijing 102249, Peoples R China
Peking Univ, Inst Energy, Beijing 100871, Peoples R China
State Key Lab Shale Oil & Gas Enrichment Mech & E, Beijing 100083, Peoples R China
PetroChina Zhejiang Oilfield Co, Res Inst Petr Explorat Dev, Hangzhou, Zhejiang, Peoples R China
Keywords NUCLEAR-MAGNETIC-RESONANCE
ARGILLACEOUS DOLOMITE RESERVOIR
PORE STRUCTURE
MERCURY INTRUSION
ORDOS BASIN
TARIM BASIN
FIELD
SANDSTONE
POROSITY
ROCKS
Issue Date Jul-2021
Publisher MARINE AND PETROLEUM GEOLOGY
Abstract Fluorescence thin section and scanning electron microscopy (SEM) analysis were performed to delineate pore spaces and pore network assemblages of oil shales of Member 2 of Paleogene Funing Formation (E(1)f(2)) in Subei Basin, China. Nuclear magnetic resonance (NMR) T-2 (transverse relaxation time) spectra were used to gain insight into pore size distribution. Fractal analysis was performed on the NMR T-2 spectra measured at saturated and centrifugal status, respectively, with the aim to reveal the different fractal behaviors of irreducible pore realms (centrifugal T-2 spectrum) and the entire pore systems (saturated T-2 spectrum). Relationships between NMR parameters and fractal dimensions were revealed. The results show that the pore spaces consist of 1) large pore realms including interparticle pores, and microfractures, 2) small pore realms including intragranular dissolution pores, intercrystal micropores and organic matter pores. The T-2 spectra are mostly bimodal and left-skewed due to abundance in small pore realms. The right peak or tail distribution is associated with large pore realms. Fractal analysis performed on saturated and centrifugal T-2 spectra show that fractal dimensions calcu-lated from centrifugal T-2 spectrum are higher. In addition, fractal dimensions for centrifugal T-2 spectrum show negative correlation relationships with BVI and T-2cutoff values. The different fractal behaviors of saturated and centrifugal T-2 spectra reflect the complex pore assemblages in oil shales. The small pore realms determine the microscopic complexity, while large pore realms control the macroscopic reservoir quality of oil shales. However large pore realms (interparticle pores and micro-fractures) are not self-similar with the small pore realms, and can't be described by fractal dimension. Fractal analysis gives insights in the heterogeneous assemblage of pore systems and helps describe complexity of pore structure.
URI http://hdl.handle.net/20.500.11897/614635
ISSN 0264-8172
DOI 10.1016/j.marpetgeo.2021.105069
Indexed SCI(E)
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