Philip A. Allen mainly investigates Paleontology, Geomorphology, Tectonics, Structural basin and Foreland basin. His study in Glacial period, Sedimentary rock, Molasse, Rift and Onlap is done as part of Paleontology. His Geomorphology research focuses on Progradation, Tectonic subsidence, Landslide, Sediment transport and Sediment.
He focuses mostly in the field of Tectonic subsidence, narrowing it down to topics relating to Back-stripping and, in certain cases, Basin modelling, Petrology and Lithospheric flexure. His study in Tectonics is interdisciplinary in nature, drawing from both Bedrock and Fluvial. His biological study spans a wide range of topics, including Sedimentary basin, Thrust fault and Unconformity.
Paleontology, Cognition, Developmental psychology, Geomorphology and Cognitive psychology are his primary areas of study. Sedimentary rock, Structural basin, Glacial period, Foreland basin and Unconformity are among the areas of Paleontology where the researcher is concentrating his efforts. His Developmental psychology research is multidisciplinary, incorporating elements of Visual search, Perception and Audiology.
Geomorphology is frequently linked to Tectonics in his study. The concepts of his Cognitive psychology study are interwoven with issues in Stimulus and Psychological refractory period. His work carried out in the field of Sediment brings together such families of science as Routing and Grain size.
His primary scientific interests are in Cognitive psychology, Sediment, Chiari malformation, Cognition and Sedimentary depositional environment. His Cognitive psychology research incorporates themes from Emotional valence, Lexical access, Perception and Priming. The various areas that Philip A. Allen examines in his Sediment study include Sedimentary rock, Hydrology, Routing and Grain size.
His Sedimentary rock study integrates concerns from other disciplines, such as Snowball Earth, Glacial period and Horizon. His Cognition research is multidisciplinary, incorporating elements of Audiology and Information processing. His Sedimentary depositional environment research is covered under the topics of Geomorphology and Paleontology.
His primary areas of study are Sediment, Sedimentary depositional environment, Geomorphology, Sediment transport and Structural basin. His Sediment study combines topics from a wide range of disciplines, such as Sedimentary rock, Soil science, Routing and Grain size. His Sedimentary depositional environment study contributes to a more complete understanding of Paleontology.
His research in Paleontology is mostly focused on Geologic record. Philip A. Allen studies Sedimentary basin which is a part of Structural basin. His biological study deals with issues like Foreland basin, which deal with fields such as Sequence stratigraphy.
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Basin Analysis: Principles and Application to Petroleum Play Assessment
Philip A. Allen;John R. Allen.
(2013)
Basin Analysis: Principles and Applications
Philip A. Allen;John R. Allen.
(1990)
Sediment flux from a mountain belt derived by landslide mapping
Niels Hovius;Colin P. Stark;Philip A. Allen.
Geology (1997)
Earth Surface Processes
Philip A. Allen.
(1997)
From landscapes into geological history
Philip A. Allen.
Nature (2008)
Anxiety Reduction through Detachment: Subjective, Physiological, and Neural Effects
Raffael Kalisch;Katja Wiech;Hugo D. Critchley;Ben Seymour.
Journal of Cognitive Neuroscience (2005)
Simulation of Foreland Basin Stratigraphy using a diffusion model of mountain belt uplift and erosion: An example from the central Alps, Switzerland
Hugh Sinclair;B. J. Coakley;P. A. Allen;A. B. Watts.
Tectonics (1991)
Evolution of the Longmen Shan Foreland Basin (Western Sichuan, China) during the Late Triassic Indosinian Orogeny
L. Yong;P. A. Allen;A. L. Densmore;X. Qiang.
Basin Research (2003)
Tides and Waves
Philip A. Allen.
(2009)
New U-Pb zircon dates for the Neoproterozoic Ghubrah glaciation and for the top of the Huqf Supergroup, Oman
Martin Brasier;Gretta McCarron;Robert Tucker;Jonathan Leather.
Geology (2000)
Experimental Aging Research
(Impact Factor: 1.652)
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