Bill D. Black, William R. Lund, David P. Schwartz, Harold E. Gill, Bea H. Mayes. Paleoseismology of Utah, volume 7 Unit 5 COLLUVIAL WEDGE - Sandy silt with gravel (SM); brownish yellow (10YR 6/6); maximum clast size 40 mm; ...
... p. m.-2:30 p. m. Das, B. M., 1984, Principles of foundation engineering:Brooks/ Cole Engineering Division of Wedsworth, Inc., Belmont, Calif., 595 p. Davidson, E. S., 1967, Geology of the Circle Cliffs area, Garfield and Kane ...
amount of syntectonic sedimentation at the front of the wedge. marizes the main parameters and results for the four series ... Series I experiments were simple, doubly vergent wedges formed from a constant thickness sand pack (Table 1).
This thesis addresses long-standing controversies surrounding normal faults that initiate and slip at low-angles (30°) and are responsible for extreme crustal extension (100%).
Trench 3 contains three zones of concentrated deformation. Fault zone 1 (FZ1 on figure 28) consists of two normal faults that underlie 8-meter-high Scarp G at the east end of the trench. The eastern fault has 3 meters of throw on unit ...
The authors would also like to thank Western Geoco for providing the Ship Shoal threedimensional seismic cube and JRS ... Genetic stratigraphic sequences in basin analysis II: application to northwest Gulf of Mexico Cenozoic basin.
Such systems may region ( critical for petroleum exploration ) ; occasionally be rejuvenated by earthquake reoccurfaults may affect later joint development and rence . joints may affect later fault growth , and their The maps in Figure ...
Black, B.D., Lund, W.R., Schwartz, D.P., Gill, H.E. and Mayes, B.H., 1996, Paleoseismic investigation on the Salt Lake City segment of the Wasatch fault zone at the South Fork Dry Creek and Dry Gulch sites, Salt Lake County, Utah: Utah ...