2015) studied the behavior of circular tunnels crossing active normal and reverse fault
rupture with different earthquake magnitudes and fault dip angles.
Along its entire map trace the fault appears as a high-angle reverse fault
with its eastern block up thrown towards west.
However, in this paper we show that the LTF is a left-lateral reverse fault
, highly dipping to the SE with a strike and a style of deformation which differ from the Carrascoy Fault, suggesting an independent kinematic behaviour.
Main Zagros Reverse Fault
is a structural boundary changes in depositional history, geography and seismicity has been proposed in the past.
The mineralization occurs along a reactivated fault, the Stuart Fault, within the regional Mount Dore Shear Zone, which is a major crustal mineralizing reverse fault
hosting the Stuart, Selwyn (approximately 8km to the Selwyn Project area), Mount Dore, Mount Elliot and Kuridala deposits.
STEP 4: For Sample B, create a reverse fault
(see diagram B): Cut through the sample at an angle.
The main part of the fault, an approximate 50 km-long section running from the NW to the central part of the fault strand, showed major displacement that was dominated by reverse fault
Moreover, two minor east-striking reverse fault
planes plastered with calcite slickenfibers were identified in Mississippian rocks of the nearby Saint-Jules-de-Cascapedia quarry (Fig.
At Porter Gap, where the lineament is the Chickasaw Bluffs, reflectors at 100--200 m depth dip west beneath the bluff face, and a steep reverse fault
underlies the base of the bluff.
Results from the drilling indicate that gold and copper mineralization is present in the hanging wall of a brittle reverse fault
that placed deformed, mafic volcanic rocks over younger, fine grained epiclastic sedimentary rocks.
While, it moves inversely, by the reverse fault
It is a N-S to NNE trending reverse fault
, placing the Carboniferous to Permian black shales on top of the Permo-Triassic volcanic rocks in its northern segment, and a Triassic intrusive over the Lower Paleozoic metamorphic rocks in the south (Fig.