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Delfin Basin
Why Did the Southern Gulf of California Rupture So Rapidly?—Oblique Divergence Across Hot, Weak Lithosphere Along a Tectonically Active Margin
Patricia Persaud
UNIVERSITY of CALIFORNIA, SAN DIEGO Marine Geophysical Study
Redalyc.Attenuation of Coda Waves in the Central Region of the Gulf Of
Space Geodetic Observation of the Deformation Cycle Across the Ballenas Transform, Gulf of California Christina Plattner University of Miami
The Structural Evolution of Pull-Apart Basins in Response to Changes in Plate Motion
Source Characteristics of the Mw 6.2 Loreto Earthquake of 12 March 2003 That Occurred in a Transform Fault in the Middle Of
Shear Wave Splitting and Mantle Flow in Mexico: What Have We Learned?
Preliminary Report on Seismological and Geotechnical Engineering Aspects of the April 4 2010 Mw
CRUSTAL STRUCTURE of the SALTON TROUGH: CONSTRAINTS from GRAVITY MODELING a Thes
The 3 August 2009 Mw 6.9 Canal De Ballenas Region, Gulf of California
Volcanic Markers of the Post-Subduction
Attenuation of Coda Waves in the Central Region of the Gulf of California, México
A BRIEF GEOLOGIC HISTORY of NORTHWESTERN MEXICO © Richard C
Paleomagnetic Quantification of Neogene Block Rotations Within an Active Transtensional Plate Boundary, Baja California Sur, Mexico
Alvin See Also
Active Tectonics in the Gulf of California and Seismicity (M N 3.0) for the Period 2002–2014
Constraints on Crust and Upper Mantle Velocities Beneath the Gu
Top View
Oblique Rifting Ruptures Continents: Example from the Gulf of California Shear Zone
Salton Trough and Northern Gulf of California
Systematic Heat Flow Measurements Across the Wagner Basin, Northern
Redalyc.Shear Wave Splitting and Mantle Flow in Mexico: What Have
Rupturing Continental Lithosphere in the Gulf Of
Inception of the Eastern California Shear Zone and Evolution of the Pacific-North American Plate Boundary
A Marine Geophysical Study of Vizcaino Bay and the Continental Margins of Western Mexico Between 27° and 30° North Latitude
Ridge-Trench Interactions and the Neogene Tectonic Evolution of The