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Facies Characteristics of Deep-lake Shales in the Sweet-pot Intervals of the Second Member of Funing Formation in Qintong Sag of Subei Basin, China and Their Controlling Factors(PDF)

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

Issue:
2025年第05期
Page:
929-943
Research Field:
沉积地质与油气勘探
Publishing date:

Info

Title:
Facies Characteristics of Deep-lake Shales in the Sweet-pot Intervals of the Second Member of Funing Formation in Qintong Sag of Subei Basin, China and Their Controlling Factors
Author(s):
WU Gong-yi1* TAN Ming-xuan2 ZHANG Yong1 WANG Jing1 CHEN Mian-pei2 ZHANG Peng-hui2 WU Feng2 WANG Xin-shuo2
(1. Taizhou Oil Production Plant, East China Oil and Gas Company, SINOPEC, Taizhou 225300, Jiangsu, China; 2. College of Oceanography, Hohai University, Nanjing 210098, Jiangsu, China)
Keywords:
mudstone and shale lithofacies characteristic sedimentary process controlling factor rift basin Funing Formation Subei Basin
PACS:
P618.13
DOI:
10.19814/j.jese.2024.09031
Abstract:
Significant breakthroughs have been made in shale oil exploration in the second member of Funing Formation in Qintong sag of Subei Basin. The sweet spot intervals are composed of deep lacustrine shale reservoirs, which exhibit strong heterogeneity, limiting the effective prediction of sweet spot distribution and resource potential evaluation. To clarify the lithofacies diversity and genetic mechanisms of deep lacustrine shale within the sweet spot intervals, multiple research methods, including key well core analysis, thin section observation, whole-rock X-ray diffraction(XRD), and automated quantitative mineralogical analysis, were employed to analyze the shale lithofacies types, genetic mechanisms, and controlling factors. The results show that according to the lithofacies classification criteria of mineral composition and sedimentary structure, the target interval of shales in the study area can be categorized into five main types, including massive mudstone facies, thin-laminated shale facies, thick-laminated shale facies, deformed-laminated shale facies, and cross-laminated shale facies, and these primary facies are further subdivided into 14 subtypes; facies association indicates that various fine-grained sedimentary processes occur in the deep lacustrine settings in the second member of Funing Formation, including suspension, flocculation, and chemical precipitation in still water, deep-water fine-grained gravity flows with rheological variations, frequent paleo-seismic activity, and substantial reworking by lake-bottom currents; the spatial variation of deep sag and fault scarp is strongly related to the elongated structure of the small lacustrine rift basin and the transport distance of terrigenous detrital materials.

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Last Update: 2025-10-01