Application of Hyperspectral Scanning in Mineral Composition Analysis of Carbonate Rocks

ZHANG Qiyan; SHI Weixin; LIU Xiao; HUI Guangji; YUAN Chunyu

doi:10.15898/j.cnki.11-2131/td.202112100200

Rock and Mineral Analysis > 2022 > 41(5): 815-825. > DOI: 10.15898/j.cnki.11-2131/td.202112100200

ZHANG Qiyan, SHI Weixin, LIU Xiao, HUI Guangji, YUAN Chunyu. Application of Hyperspectral Scanning in Mineral Composition Analysis of Carbonate Rocks[J]. Rock and Mineral Analysis, 2022, 41(5): 815-825. DOI: 10.15898/j.cnki.11-2131/td.202112100200

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Application of Hyperspectral Scanning in Mineral Composition Analysis of Carbonate Rocks

Core and Samples Center of Land and Resources, Beijing 100083, China

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Received Date: December 09, 2021
Revised Date: March 01, 2022
Accepted Date: March 12, 2022
Available Online: November 10, 2022

Abstract

HIGHLIGHTS
(1) Hyperspectral scanning can be used to quickly and efficiently interpret the characteristics and changes of mineral composition in the longitudinal direction of the core.

(2) QEMSCAN can be used to finely depict and quantitatively analyze the mineral composition, content and micro characteristics of the core.

(3) The two methods are combined to study the spatial changes of mineral composition and microscopic characteristics at different levels. Good results have been achieved.

ABSTRACT

BACKGROUND
Mineral composition and its microscopic characteristics are of great significance to the study of sedimentary environment, rock framework and reservoir space of oil and gas reservoirs.
OBJECTIVES
To investigate the mineral composition, content and spatial distribution of carbonate core samples of the Permian Longge Formation and provide the basis for oil and gas evaluation of the Paleozoic carbonate reservoirs in Qiangtang Basin.
METHODS
The sample was analyzed by hyperspectral scanning and QEMSCAN.
RESULTS
The Longge Formation is dominated by microcrystalline limestone and granulated limestone, and the minerals are mainly calcite and dolomite, the contents of which are generally greater than 90%, followed by quartz and a minor clay mineral and feldspar. The mineral composition has obvious characteristics of longitudinal segmentation. The contents of calcite and dolomite are higher in the upper section. The content of dolomite in the middle section is higher, and the degree of dolomization is relatively strong. The porosity and permeability of this section have decreased. The lower section is mainly composed of calcite. In addition, the analysis of clay mineral characteristics shows that the Longge Formation has experienced complex sedimentary-diagenesis and late thermal disturbance and fluid replacement, which has a strong impact on oil and gas migration and preservation in this area.
CONCLUSIONS
Hyperspectral scanning technology can be used to quickly and efficiently interpret large-scale mineral features. QEMSCAN enables more precise and quantitative analysis of mineral microscopic features. The Longge Formation is dominated by carbonate and obviously affected by diagenesis and the local dolomization is strong. The oil and gas conditions in this formation are poor.
- mineral composition,
- hyperspectral scanning,
- QEMSCAN,
- carbonate rock,
- Permian Longe Formation

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Application of Hyperspectral Scanning in Mineral Composition Analysis of Carbonate Rocks