Influence of detrital composition on the diagenetic history of tight sandstones with implications for reservoir quality: Examples from the Permian Xiashihezi Formation and Carboniferous Taiyuan Formation, Daniudi gas field, Ordos Basin, China. (December 2017)

• Record Type: Journal Article
• Authors: Xu, Ningning; Qiu, Longwei; Eriksson, Kenneth A.; Klyukin, Yury Igorevich; Wang, Yang; Yang, Yongqiang
• Is Part Of: Marine and petroleum geology. Volume 88(2017)
• Page Start: 756
• Page End: 784
• Publication Date: 2017-12
• Subjects: Ordos basin -- Upper Paleozoic -- Tight gas sandstones -- Diagenesis -- Secondary pores -- K-feldspar dissolution -- Illitization; Submarine geology -- Periodicals; Petroleum -- Geology -- Periodicals; Géologie sous-marine -- Périodiques; Pétrole -- Géologie -- Périodiques; Petroleum -- Geology; Submarine geology; Periodicals; Electronic journals; 551.468
• DOI: 10.1016/j.marpetgeo.2017.09.018
• Languages: English
• ISSNs: 0264-8172

Abstract

Abstract: Tight-gas reservoirs, characterized by low porosity and low permeability, are widely considered to be the product of post-depositional, diagenetic processes associated with progressive burial. This study utilizes a combination of thin section petrography, scanning electron microscopy, microprobe and back scatter electron analysis, stable isotope geochemistry and fluid inclusion analysis to compare the diagenetic history, including porosity formation, within sandstones of the second member of Carboniferous Taiyuan Formation (C3 t2 ) and the first member of Permian Xiashihezi Formation (P1 x1 ) in the Ordos Basin in central China. In the P1 x1 member, relatively high abundances of metamorphic rock fragments coupled with a braided river and lacustrine delta environment of deposition, produced more smectite for transformation to illite (50–120 °C). This reaction was driven by dissolution of unstable minerals (K-feldspar and rock fragments) during the early to middle stages of mesodiagenesis and consumed all K-feldspar. Abundant intragranular porosity (average values of 2.8%) and microporosity in kaolinite (average values of 1.5%) formed at these burial depths with chlorite and calcite developed as by-products. In the C3 t2 member, relatively low abundances of metamorphic rock fragments coupled with an incised valley-coastal plain environment of deposition resulted in less smectite for transformation to illite. High K + /H + ratios in the early pore waters related to a marine sedimentary environment of deposition promoted this reaction. Under these conditions, K-feldspar was partially preserved. During the middle to late stages of mesodiagenesis, K-feldspar breakdown produced secondary intragranular (average values of 1.4%) and intergranular pores (average values of 1.2%). Release of K + ions promoted illitization of kaolinite with quartz overgrowths and ferrous carbonates developed as by-products. This study has demonstrated that whereas both members are typical tight-gas sandstones, they are characterized by quite different diagenetic histories controlled by the primary detrital composition, especially during mesodiagenesis. Types of secondary porosity vary between the two members and developed at different stages of progressive burial. The content of unstable detrital components, notably feldspar, was the key factor that determined the abundance of secondary porosity. Highlights: Inferring the primary composition of tight gas sandstones based on point-counting of replacement products of feldspar. Contrasting the paragenetic histories of two upper Paleozoic reservoirs using a combination of analytical methods. Explaining and contrasting the types, timing and formation mechanisms of secondary porosity in the two members.