Controlling factors of acoustic properties in continental carbonates: Implications for high-resolution seismic imaging. (March 2022)

• Record Type: Journal Article
• Authors: Bailly, C.; Kernif, T.; Hamon, Y.; Adelinet, M.; Fortin, J.
• Is Part Of: Marine and petroleum geology. Volume 137(2022)
• Publication Date: 2022-03
• Subjects: Continental carbonates -- Paludal tufa -- Palustrine environment -- Diagenesis -- Multi-scale porosity -- Acoustic properties -- Synthetic seismic -- Seismic interpretation; 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.2021.105518
• Languages: English
• ISSNs: 0264-8172

Abstract

Abstract: Continental carbonates are characterized by multi-scale heterogeneous porous networks, making the geological interpretation of seismic imaging difficult. We investigate two sedimentary sections exhibiting a similar facies succession, combining geological characterizations and multi-scale acoustic measurements. Based on outcrop investigation and petrographic description, we define nine sedimentary facies displaying contrasted early diagenetic evolutions. According to the vertical facies variations, we develop a depositional model corresponding to a low gradient valley fed by freshwaters, subdivided into three main domains (alluvial plain, palustrine and paludal). To understand the acoustic properties of the studied sedimentary rocks while remaining representative of their multi-scale heterogeneity, we acquire acoustic measurements at two different scales: i) at log-scale, directly on the outcrop surfaces using a frequency of 250 kHz; and ii) at plug-scale as usually done in laboratory using a frequency of 500 kHz. Based on these multi-scale geophysical acquisitions, we link in-situ P-wave velocities with the different sedimentary facies while characterizing centimeter-scale Representative Elementary Volumes (REVs). Conversely, based on laboratory measurements and thin-section petrography, we define relationships between P-wave velocity, porosity, facies, and diagenesis, corresponding to millimeter-scale REVs. Using both in-situ P-wave velocity measurements and plug densities, we construct 1-D synthetic seismograms showing meter-scale seismic reflectors equivalent to crosswell seismic frequency ranges. This approach shows the following: i) high-amplitude seismic reflectors fit with facies changes associated to diagenetic contrasts ( e.g. cemented versus uncemented carbonates); ii) reflection free-zones match with a succession of facies changes affected by diagenetic homogenization ( e.g. intensely to pervasively recrystallized and cemented carbonates). Our work highlights the importance of relating an extensive geological description of carbonates (facies, depositional model, diagenesis) together with multi-scale acoustic measurements and synthetic seismic modelling to predict the high-resolution heterogeneities of subsurface reservoirs. Graphical abstract: Image 1 Highlights: Investigation of palustrine and paludal tufa carbonates. Facies and diagenetic characterizations of heterogeneous porous carbonates. Multi-scale measurements of P-wave velocity in the laboratory and on outcrop. Geological significance of synthetic seismograms equivalent to crosswell seismic. Seismic imaging of continental carbonates is strongly controlled by diagenesis.