A transfer zone is a kind of structure that is produced to conserve deformation of a fault
structure on both sides. Increasing numbers of transfer zones are being identified in rift …

孤店断陷为松辽盆地南部深层天然气勘探的有利区带, 同时也记录了中国东部中-
新生代板块运动和盆地演化的丰富信息. 利用钻测井资料及高分辨率三维地震资料 …

Normal faults grow via a sympathetic increase in their displacement and length ('isolated
model') or by rapid establishment of their near-final length prior to significant displacement …

Catchments provide water and sediment to downstream sedimentary systems, and these
form individual source-to-sink systems. Source-to-sink systems comprise adjacent linked …

Throw-distance (TD) and throw-depth (TZ) plots are widely used by researchers and industry
to examine the growth of normal faults. This study uses high-quality three-dimensional (3D) …

Individual sandstone beds containing a co-genetic mud-clast-rich (MCR) division are being
increasingly described from the distal reaches of many deep-water fan systems. These …

Structurally controlled bathymetry in rifts has a significant influence on sediment routing
pathways and depositional architecture of sediment gravity flow deposits. In contrast to rift …

The Gulf of Suez–Red Sea rift system exhibits superb outcrop examples of extensional
transfer zones and displays the control of these zones on syntectonic and post-tectonic …

High-quality three-dimensional (3D) seismic reflection and borehole data from the Egersund
Basin, offshore Norway are used to characterise the structural style and determine the timing …

Sea‐floor topography of deep‐water folds is widely considered to have a major impact on
turbidity currents and their depositional systems, but understanding the flow response to …