The Kutch basin is a western margin pericratonic rift basin of India. Nagar Parkar uplift in the north and Kathiawar uplift (Saurashtra horst) in the south respectively along Nagar Parkar …
CK Morley, RA Nelson, TL Patton… - AAPG …, 1990 - pubs.geoscienceworld.org
Transfer zones in extensional regions display a wide range of geometries from discrete fault zones to zones of broad warping. The classification of extensional fault displacement …
The Dharwar craton comprises two distinct parts separated by a steep N–S sinistral shear zone. In the western part a pre-2900Ma complex of orthogneisses, granodiorites and narrow …
G Stampfli, J Marcoux, A Baud - Palaeogeography, Palaeoclimatology …, 1991 - Elsevier
Rifting processes, leading to sea-floor spreading, are characterized by a sequence of events: transtensive phase of extension with syn-rift volcanism; simple shear extension …
The inherent asymmetry of extension by detachment leads to contrasting and conjugate classes of passive margins. Upper‐plate margins comprise crust above a deeper …
KR McClay, MJ White - Marine and Petroleum Geology, 1995 - Elsevier
The three-dimensional progressive development of orthogonal and oblique rift systems has been simulated using scaled, analogue sandbox models. The orientation, α, of the zone of …
KR McClay - Marine and petroleum Geology, 1990 - Elsevier
Scaled analogue models have provided graphic new insights into the progressive development of extensional fault systems. This paper reviews recent results of an on-going …
RB Færseth - Journal of the Geological Society, 1996 - lyellcollection.org
The main structural elements resulting from Late Permian-Early Triassic extension have been resolved across the total width of the northern North Sea. The northern segment of the …