Structural characterization of the Longyearbyen CO2 Lab reservoir-caprock succession

This baseline study on fracture populations affecting the Mesozoic sedimentary succession of central Spitsbergen (Svalbard) has been performed to characterize the reservoir-caprock system explored for potential subsurface CO2 storage by the Longyearbyen CO2 Lab project. Integrating structural and st...

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Bibliographic Details
Published in:Proceedings, Fourth EAGE CO2 Geological Storage Workshop
Main Authors: Ogata K., Senger K., Braathen A., Olaussen S., Tveranger J.
Other Authors: Ogata, K., Senger, K., Braathen, A., Olaussen, S., Tveranger, J.
Format: Conference Object
Language:English
Published: European Association of Geoscientists and Engineers, EAGE 2014
Subjects:
Svalbard
Longyearbyen
Spitsbergen
Online Access:http://hdl.handle.net/11588/820211
https://doi.org/10.3997/2214-4609.20140116
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Summary:This baseline study on fracture populations affecting the Mesozoic sedimentary succession of central Spitsbergen (Svalbard) has been performed to characterize the reservoir-caprock system explored for potential subsurface CO2 storage by the Longyearbyen CO2 Lab project. Integrating structural and stratigraphie analyses of outcrop and borehole data, we identified recurrent litho-structural and structural units (LSUs and SUs, respectively) on the basis of their fracture associations, lithologies and dominant sedimentary facies. A principal fracture settrending approximately E-W (J1) and a subordinate fracture set trending approximately N-S (J2) have been recognized. Subordinate systems of shear fractures (SI) trending roughly NE-SW and NW-SE, and a secondary low-angle, fracture set (S2) striking E-W to NW-SE have been observed. Their origin is interpreted as related to the far-field stress of the Paleogene West Spitsbergen fold-and-thrust Belt. The identified units are thought to influence the local hydrogeologic regime due to the intrinsic variations in the matrix and fracture network properties. The architecture of the reservoir-caprock succession is segmented, with the vertical alternation of intervals characterized by 1) fracture porosity and permeability, 2) microfracturing- related matrix porosity, and 3) preferential subsurface fluid flow pathways. Copyright © (2014) by the European Association of Geoscientists & Engineers. All rights reserved.

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