Morphology of the Blanco Transform Fault Zone-NE Pacific: Implications for its tectonic evolution
- 1 March 1992
- journal article
- Published by Springer Science and Business Media LLC in Marine Geophysical Research
- Vol. 14 (1), 25-45
- https://doi.org/10.1007/bf01674064
Abstract
No abstract availableKeywords
This publication has 60 references indexed in Scilit:
- Kinematics of overlapping rift propagation with cyclic rift failureEarth and Planetary Science Letters, 1990
- A compendium of causes and effects of processes at transform faults and fracture zonesReviews of Geophysics, 1987
- Bookshelf tectonics: Rotated crustal blocks within the Sovanco Fracture ZoneGeophysical Research Letters, 1986
- Quantitative methods for analyzing the roughness of the seafloorReviews of Geophysics, 1985
- A tectonic model for ridge-transform-ridge plate boundaries: Implications for the structure of oceanic lithosphereTectonophysics, 1984
- Evolution of pull‐apart basins and their scale independenceTectonics, 1982
- Near-Bottom Reconnaissance of a Fast-Slipping Transform Fault Zone at the Pacific-Nazca Plate BoundaryThe Journal of Geology, 1978
- Are spreading centers perpendicular to their transform faults?Nature, 1977
- Serpentinite protrusions in the oceanic crustEarth and Planetary Science Letters, 1976
- MAGNETIC SURVEY OFF THE WEST COAST OF NORTH AMERICA, 40° N. LATITUDE TO 52° N. LATITUDEGSA Bulletin, 1961