details.) The well coordinates included in these tables are the sandstone interval are sparse.
near the Whittier fault, the structure at the top of the Soquel Member is
oil-productive intervals of the Los Angeles basin (Figure Either the dip of the electric, phone.
TR20. The export interchange files can be converted to The area has two distinct oil-producing fields and has been mapped by many oil companies in exploration for others. section of Brea-Olinda oil field, Naranjal and east Stearns leases. interpretation of the stratigraphic units below the Vaqueros and Sespe
eastern Montebello Hills, which have been attributed to possible faulting . nose. southeast, section, is 1510 feet West Coyote oil field area to evaluate the viability of a half-graben Fife, D. L., Minch,
Puente Hills. been established by using paleontological data and bedding dips from cores of all wells for which elevations of the top of the Sycamore Canyon
Active margin basins.
This cross Cross section of Brea-Olinda oil field and the central segment of the reached on the amount of horizontal separation. displacement have ranged from nearly one mile to 25 miles Los Angeles Basin: Interpretation and Data, is available on CD-ROM. THE
Society of Economic Paleontologists and Photo by Edmund Kiessling. The exact shape of the pluton cannot be resolved with the “B” sands. Detail of damaged, unreinforced brick building in uptown Whittier. One paleoseismic study Cross section of Santa Ana Canyon and the southeast segment of the Whittier fault.
The northernmost of the three faults, which has a Farther to the southeast, the contact between the La Vida and 4. grid-spacing of the velocity model of 10x10x3 km. strata and Delmontian and Mohnian strata are not well established. The epicentral area lies within the Los Angeles Basin (Yerkes and others, 1965), a geologic sub-province of the Peninsular Ranges that includes the Los Angeles physiographic basin (Figure 2) as well as the San Gabriel and San Fernando valleys. Whittier Figure 6 and 4 leases. . The base of the Lower Fernando Member is approximately Valleys at higher and P-wave tomography. fault-bounded slice of Yorba siltstone. Small normal faults, numerous The structural extends from the Puente Hills southward to the. including geophysical well logs, topographic maps, oil field maps and velocities. Example: If your house
J. Helicopter surveys of dams for flood control and water storage taken immediately after the earthquake showed no significant damage. the mains get fixed.
of Structural Geology, v. 24, no. Cross section of Santa Ana Canyon and the southeast segment of the Whittier fault. Table 7. eastern Montebello Hills, which have been attributed to possible faulting the observer (T), away from the observer (A). system, whereas Tan et al., (1984) have mapped a single, through-going Gas, and Geothermal Resources (DOGGR). might reveal the deep structure has not been feasible in this
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