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Our study focuses on a region of the basin where two non-overlapping fault segments are separated by a transfer zone.
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The typical rift system geometry was characterised by two offset rift segments connected by a major transfer zone in which boundary faults were oblique to the extension vector and displayed a significant transcurrent component of movement.
In case of staircase offset of the rift segments (φ=90°), the structural pattern was characterised by two isolated rift depressions linked by a narrow transfer zone in which border faults with alternating polarity overlapped.
This new explorative milieu would function as a transfer-zone between academia, economy, and society.
Structural framework across the sub-basin reveals that the most remarkable tectonic setting is represented by the central transfer zone (CTZ) which divides the sub-basin into two independent depressions, and two kinds of sequence architectures are summarized: (i) the western multi-stage faults slope; (ii) the eastern flexure slope break belt.
A heat transfer zone physical model is proposed for programming.
This, here designed as the Scicli Line Fault Belt, is composed of two N50 oriented extensional basins that, linked by a regional N10 trending transfer zone, originated during the Early Pleistocene and experienced, since the Late Quaternary, a positive tectonic inversion.
In regeneration experiments, a loss of sorption performance was observed during seven cycles of sorption desorption indicated by a shortened breakthrough time and a broadened mass transfer zone.
The cavity zone is an important mass transfer zone of a RPB.
Its zone between the packing and the casing (cavity zone) is an important mass transfer zone.
The western branch comprises deep rift basins separated by transfer zones, commonly localised onto pre-existing structures, offering good regional scale hydrocarbon traps.
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