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The Diagenesis of Sandstone of the Upper Paleozoie, Da-22 Well Field of Tabamiao Area, North Ordos Basin
Author: WeiWenWen
Tutor: HuangSiJing
School: Chengdu University of Technology
Course: Geology
Keywords: Ordos Basin Upper Paleozoic strata Carbonate cements Dissolution Diagenesis
CLC: P618.13
Type: Master's thesis
Year: 2011
Downloads: 42
Quote: 0
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Abstract
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The paper mainly discusses the control factors of the Ordos Basin Tabamiao Upper Paleozoic sandstone diagenesis . 29 samples into the thin section analysis and identification , to determine detrital grains and authigenic mineral composition and content . Paragenetic sequence carefully study the distribution of authigenic minerals . Upper Paleozoic sandstone of the Ordos Basin Tabamiao area rich phyllite and mudstone plastic characteristics , which makes the strong compaction deformation early significant densification . Its relatively high content of cuttings is the parent rock source area rich metamorphic rocks by strong acidic water corrosion and reform of the coal-bearing strata during diagenesis . Basis placeholder relations and mineral type and morphology , identified a different type of carbonate rocks cement . C-I type calcite filling intergranular porosity formed earlier . Can be divided into the C - IA -type and C-Ib type in which the C - Ia Calcite mainly formed in a segment too , may BSR ( bacterial reduction of sulfate) with the product . C-Ib - type calcite formation interbedded with coal-bearing strata in the formation process of the peat role of organic acids , carbon dioxide Feldspar dissolution of calcite formation . C-II type calcite formed in the plastic debris compaction deformation may enter the diagenetic evolution stage in coal-bearing strata formed CO 2 formation of feldspar dissolved calcite cement . The DI type dolomite diagenetic unclear , deep burial formed under relatively alkaline environment . D-II dolomite shaped paralic the phase mixing water environment extensively developed . The authigenic quartz identified two types , respectively, is Q-1 and Q -2 . Q-1 quartz cement euhedral its formation requires a higher pore space , may be the dissolution Dissolution and alteration of the sandstone . Q-2 type euhedral difference reflects the region generally strongly authigenic quartz precipitation space compaction is suppressed . Identified two dissolution based on the characteristics of secondary porosity . Combination of burial characteristics of the coal-bearing strata to recognize that the first phase of dissolution occurred earlier , may be associated with interbedded coal-bearing strata in the formation process of the peat role of organic acids , carbon dioxide -related . Second phase dissolution occurs relatively late diagenetic evolution stage may be entering with the coal-bearing strata to form CO 2 .
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