TITLE:
Fracture Permeability: Outcrop Analogues from Active Plate Boundaries and Intraplate Contexts of Iceland
AUTHORS:
Maryam Khodayar, Sveinbjörn Björnsson
KEYWORDS:
Fracture Permeability, Fluid Flow, Fractured Reservoirs, Rift Zone, Transform Zone, Tectonic of Iceland
JOURNAL NAME:
Open Journal of Geology,
Vol.11 No.12,
December
9,
2021
ABSTRACT: We bring new insights into fracture permeability with 7 analogues from the intraplate outcrops of West Iceland (WI), the active South Iceland transform zone (SISZ), the intersection of rift and SISZ near Hengill (Reykjafjall-RF), and the Reykjanes oblique rift (RP). WI formed at Tertiary plate boundaries, shifted away, is now cut by the Quaternary intraplate Snæfellsnes volcanic zone (SVZ), and undergoes occasional earthquakes. By contrast, fractures are being formed and reactivated under intense plate boundary earthquakes in the younger SISZ, RF and RP. Our mapping of stratigraphy, basement fractures, surface ruptures of earthquakes, and leakages of cold and hot water in all areas shows that: 1) In active SISZ, RF and RP, permeable fractures are identical to N-S to NNW dextral, ENE to E-W sinistral, and WNW to NNW sinistral source faults of earthquakes, acting as Riedel shears that accommodate the sinistral motion of the transform zone. The NNE/NE rift-parallel extensional fractures are the least frequent permeable set. Notably, the NW and WNW sets also show dextral motions in RP where they could be splay of each other but belong to a separate developed fracture system, and in the SISZ where the NW set is a splay of a N-S source fault of earthquake. However, permeable fractures in the intraplate WI are only oblique-slip sets striking N-S to NNW dextral, ENE sinistral, and WNW dextral parallel to the SVZ. 2) In each area, the permeable sets fit the fault plane solutions of intraplate or plate boundary earthquakes, as well as the latest stress fields that allow fracture opening for fluid flow. 3) Fractures are more open in the younger SISZ, RF, and RP, with leakages along the fractures and their splays rather than by their tips or in the stepovers. In the older WI where the crust and fractures are filled with secondary minerals, leakages are as much along fractures as where numerous fracture intersections facilitate fluid flow. 4) In case of intersecting fractures, the strike and dip direction of the structures determine which set acts as a carrier or a barrier to the flow. 5) Although Iceland is more known for rifting, these analogues demonstrate that fracture permeability, block compartmentalisation, and fluid flow are controlled by the oblique-slip structures developed under transform mechanism.