The formation of the NE Atlantic conjugate margins is the result of multiple rifting phases
spanning from the Late Paleozoic and culminating in the early Eocene when breakup was …

Microcracks in fault damage zones can heal under thermally controlled processes. If a flow
communication exists between a fluid source and the fault damage zone, warm fluids can …

Like many rift basins worldwide, the Inner Moray Firth Basin (IMFB) is bounded by major
reactivated fault zones, including the Helmsdale Fault and the Great Glen Fault (GGF). The …

The laminated limestones of the Crato Formation, Araripe Basin (NE of Brazil) have been
investigated, as they are analogous to facies of the carbonate reservoirs of the pre-salt …

This study presents, for the first time in the southern Apennines (Southern Italy), evidence of
fault-driven hydrothermal dolomitization during the late Triassic rifting of the western Adria …

Faults commonly form loci for high fluid flux in sedimentary basins, where fluids, rocks and
deformation processes frequently interact. Here, we elucidate the interaction of fluid flow …

Evidence of hydrothermal activity is reported for the Mesozoic pre‐and syn‐rift successions
of the western Adriatic palaeomargin of the Alpine Tethys, preserved in the Western …

We conducted microstructural and microchemical analyses of deformation bands in a
forearc fold belt consisting of the Eocene Urahoro Group located in northern Japan. In the …

Abstract In the Maritime Alps (NW Italy-SE France), the Middle Triassic-Berriasian platform
carbonates of the Provençal Domain are locally affected by an intense hydrothermal …

The Hurricane fault is a∼ 250 km long, west-dip**, segmented normal fault zone located
along the transition between the Colorado Plateau and the Basin and Range tectonic …