His primary areas of study are Seismology, Rift, Paleontology, Crust and Continental crust. His work carried out in the field of Seismology brings together such families of science as Amplitude, Triple junction and Mineralogy. Tectonics covers Dale S. Sawyer research in Rift.
He studies Oceanic crust which is a part of Paleontology. His studies in Crust integrate themes in fields like Petrology and Graben. As a part of the same scientific family, he mostly works in the field of Continental crust, focusing on Lithosphere and, on occasion, Plate tectonics and Geodynamics.
Dale S. Sawyer focuses on Seismology, Paleontology, Rift, Crust and Continental crust. He works mostly in the field of Seismology, limiting it down to topics relating to Seafloor spreading and, in certain cases, Magnetic anomaly. His work on Sedimentary rock and Sedimentary basin as part of general Paleontology research is frequently linked to Margin, bridging the gap between disciplines.
His study on Passive margin and Volcanic passive margin is often connected to Breakup as part of broader study in Rift. His Crust research includes elements of Lithosphere, Mantle convection and Petrology. His biological study spans a wide range of topics, including Continental margin, Plate tectonics and Oceanic crust.
Dale S. Sawyer mainly investigates Seismology, Margin, Detachment fault, Reflector and Tectonophysics. Dale S. Sawyer has included themes like Transition zone, Mantle and Crust in his Seismology study. Continental crust is the focus of his Mantle research.
His Continental crust research is multidisciplinary, incorporating elements of Seafloor spreading and Oceanic crust. He undertakes multidisciplinary studies into Detachment fault and Rift in his work. His research investigates the link between Rift and topics such as Fault that cross with problems in Azimuth and Passive margin.
His primary areas of study are Seismology, Mantle, Rift, Detachment fault and Transition zone. His Mantle study frequently links to other fields, such as Crust. The study incorporates disciplines such as Geodynamics, Subduction, Mantle convection and Hotspot in addition to Crust.
Dale S. Sawyer has researched Rift in several fields, including Fault slip, Fault block, Fault and Azimuth. Dale S. Sawyer performs multidisciplinary study in Detachment fault and Continental crust in his work. His work deals with themes such as Seafloor spreading, Mid-ocean ridge and Oceanic crust, which intersect with Continental crust.
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Distribution of Crust and Early History, Gulf of Mexico Basin
Richard T. Buffler;Dale S. Sawyer.
Breakup of the Newfoundland Iberia rift
B. E. Tucholke;D. S. Sawyer;J.-C. Sibuet.
Geological Society, London, Special Publications (2007)
How preexisting weaknesses control the style of continental breakup
John A. Dunbar;Dale S. Sawyer.
Journal of Geophysical Research (1989)
Tectonosedimentary evolution of the deep Iberia‐Newfoundland margins: Evidence for a complex breakup history
Gwenn Péron-Pinvidic;Gianreto Manatschal;Tim A. Minshull;Dale S. Sawyer.
Free gas at the base of the gas hydrate zone in the vicinity of the Chile triple junction
Nathan L. B. Bangs;Dale S. Sawyer;Xenia Golovchenko.
The crust under the Gulf of Mexico basin
Dale S. Sawyer;Richard T. Buffler;Rex H. Pilger.
Assessment of crustal velocity models using seismic refraction and reflection tomography
Colin A. Zelt;Kalachand Sain;Julia V. Naumenko;Dale S. Sawyer.
Geophysical Journal International (2003)
Deep structure of the U.S. Atlantic continental margin, offshore South Carolina, from coincident ocean bottom and multichannel seismic data
W. Steven Holbrook;E. C. Reiter;G. M. Purdy;D. Sawyer.
Journal of Geophysical Research (1994)
Mechanisms of extension at nonvolcanic margins: Evidence from the Galicia interior basin, west of Iberia
M. Perez-Gussinye;M. Perez-Gussinye;César R. Ranero;Timothy J. Reston;D. Sawyer.
Journal of Geophysical Research (2003)
Continental rifting at pre-existing lithospheric weaknesses
John A. Dunbar;Dale S. Sawyer.
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