M. Wyss,Z. Lu.Plate boundary segmentation by stress directions: southern San Andreas fault, California. Geophysical Research Letters . 1995Wyss M and Lu Z (1995). Plate boundary segmentation by stress directions
Jachens, R.C., and Zoback, M.L., 2000, The San Andreas Fault in the San Francisco Bay region, California; structure and kinematics of a young plate boundary: International Book Series, v. 3, p. 217-231.Jachens, R.C., and Zoback, M.L., 1999, The San Andreas fault in the San ...
Carrizo Plain National Monument San Andreas Fault (boundary between the Pacific Plate and the North American Plate) California USA North America,站酷海洛,一站式正版视觉内容平台,站酷旗下品牌.授权内容包含正版商业图片、艺术插画、矢量、视频、音乐素材、字
The San Andreas Fault is a "transform" fault. That means the two sides slide past one another. Both plates mentioned in the article are pressing against one another. Saying that a big earthquake will cause "...all of California west of the fault (to slip) into the sea,..." is like...
We performed forward modelling of seismic anisotropy beneath a migrating strike-slip plate boundary to: (1) test if such a geodynamic context might explain teleseismic shear wave splitting data in the vicinity of the central part of the San Andreas Fault and (2) constrain the power of such ...
Geodetic strain across the San Andreas Fault reflects elastic plate thickness variations (rather than fault slip rate). Earth Planet. Sci. Lett. 269, 352-365.Chery, J. (2008), Geodetic strain across the San Andreas Fault reflects elastic plate thickness variations (rather than fault slip rate)...
THE SOUTHERN SAN ANDREAS FAULT SYSTEM AND NORTHERN GULF OF CALIFORNIA: FORMATION OF NEW CRUST ALONG A TRANSTENSIONAL PLATE BOUNDARYSTOCK, Joann M
Continental transform margins are broad, complex regions dominated by strike-slip motion that mark the boundary between lithospheric plates. To better understand plate interactions at continental transforms, variations in crustal and upper mantle structure along the San Andreas transform margin have been ...
The Indio Hills wedge-shaped uplift block is located in between two boundary fault strands, the Indio Hills fault to the northeast and the main San Andreas fault to the southwest, which merge to the southeast. Uplift commenced about or later than 0.76 million years ago a...
(2) Between 37掳N and 39掳N the plate boundary (within the mantle) separating the Pacific and North American plates has developed approximately 4060 km east of the surface trace of the San Andreas fault and lies beneath the Hayward-Calaveras faults and associated faults. The surface trace of...