Patience A. Cowie focuses on Fault, Scaling, Seismology, Stress field and Geometry. While the research belongs to areas of Fault, Patience A. Cowie spends her time largely on the problem of Tectonics, intersecting her research to questions surrounding Communication channel. The various areas that Patience A. Cowie examines in her Scaling study include Geomorphology, Power law and Data set.
The Power law study combines topics in areas such as Scale, Fracture, Characteristic length, Statistical physics and Field. Her Data set study combines topics from a wide range of disciplines, such as Closed and exact differential forms and Plate tectonics. Her work on Rift is typically connected to Strain rate as part of general Seismology study, connecting several disciplines of science.
Her primary areas of study are Seismology, Fault, Geomorphology, Tectonics and Fault scarp. Her research in Fault intersects with topics in Geometry, Scaling and Rift. Her Geometry research incorporates elements of Geotechnical engineering and Range.
Her Scaling study integrates concerns from other disciplines, such as Magnitude, Statistical physics, Power law and Data set. Her Fault scarp research focuses on subjects like Ridge, which are linked to Accretion and Seafloor spreading. Her study explores the link between Bedrock and topics such as Stream power that cross with problems in Sediment transport.
Seismology, Fault, Rift, Surface and Sediment are her primary areas of study. Her study looks at the intersection of Seismology and topics like Bedrock with Seismic hazard and Paleoseismology. She has included themes like Geomorphology and Continental margin in her Fault study.
Her Rift research integrates issues from Fluvial and Subsidence. Her Surface research also works with subjects such as
Her primary areas of investigation include Seismology, Active fault, Fault, Rift and Fault scarp. Her Seismology research includes elements of Seafloor spreading and Petrology. Her research in the fields of Elastic-rebound theory overlaps with other disciplines such as Coulomb and Strain rate.
Her research investigates the connection with Fault and areas like Geomorphology which intersect with concerns in Seismic hazard and Paleoseismology. Her Rift research incorporates themes from Sediment, Fluvial and Subsidence. She has researched Fault scarp in several fields, including Bedrock, Seismic moment, Structural geology and Inversion.
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Scaling of fracture systems in geological media
E. Bonnet;O. Bour;N. E. Odling;P. Davy.
Reviews of Geophysics (2001)
Physical explanation for the displacement-length relationship of faults using a post-yield fracture mechanics model
Patience A Cowie;Christopher H Scholz.
Journal of Structural Geology (1992)
Displacement-length scaling relationship for faults: data synthesis and discussion
Patience A Cowie;Christopher H Scholz.
Journal of Structural Geology (1992)
Fault growth and fault scaling laws: Preliminary results
C. H. Scholz;N. H. Dawers;J.-Z. Yu;M. H. Anders.
Journal of Geophysical Research (1993)
Damage zone and slip-surface evolution over μm to km scales in high-porosity Navajo sandstone, Utah
Z.K. Shipton;P.A. Cowie.
Journal of Structural Geology (2001)
Determination of total strain from faulting using slip measurements
C. H. Scholz;Patience A. Cowie.
Nature (1990)
Growth of faults by accumulation of seismic slip
Patience A. Cowie;Christopher H. Scholz.
Journal of Geophysical Research (1992)
A healing–reloading feedback control on the growth rate of seismogenic faults
P.A. Cowie.
Journal of Structural Geology (1998)
Bedrock channel adjustment to tectonic forcing: Implications for predicting river incision rates
Alexander C. Whittaker;Patience A. Cowie;Mikaël Attal;Gregory E. Tucker.
Geology (2007)
A mechanism to explain rift-basin subsidence and stratigraphic patterns through fault-array evolution
Sanjeev Gupta;Patience A. Cowie;Nancye H. Dawers;John R. Underhill.
Geology (1998)
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