STYLOLITIZATION OF LATE EOCENE TO EARLY MIOCENE CARBONATE-BEARING LITHOLOGIES FROM IODP HOLE 317-U1352C (CANTERBURY BASIN)
The main focus of our study is the diagenetic aspect of pressure solution, and potentially related fracturation and cementation. Our approach has an emphasis on petrography and geochemistry. In order to gain a better understanding of the pressure solution process, the impact of several factors (such as burial depth, grain fabric and lithology and pore fluid characteristics) and the stylolite characteristics are assessed in late Eocene to early Miocene carbonate-bearing rock samples from the Integrated Ocean Drilling Program (IODP) Hole 317-U1352C (Canterbury Basin).
In addition, we assess fluid mobility during and after pressure solution. During pressure solution, carbonate is thought to dissolve, producing a fluid that could lead to fluid flow, which then could result in fluid escaping through fractures, or conversely in the cementation of pores or fractures if the fluid does not escape. Hence, we evaluate fluid flow and cementation and the role of fractures and the impact of insoluble residue along the stylolites by using a (quantitative) petrographic and geochemical approach.
A better understanding of what controls pressure solution and of the impact of stylolitization on fluid flow, derived from our study, will lead to a better prediction of diagenesis and heterogeneity in carbonate lithologies.