Preliminary Magnetostratigraphic Study of the Split Mountain and Lower Imperial Groups, Split Mountain Gorge, Western Salton Trough, CA

We present preliminary results of a magnetostratigraphic study of Miocene-Pliocene sedimentary rocks of the Split Mt. and lower Imperial Groups exposed in Split Mt. Gorge and eastern Fish Creek-Vallecito basin, western Salton Trough. Precise age control for the base of this thick section is needed to improve our understanding of the early history of extension-related subsidence in this region. The geologic setting and stratigraphic framework are known from previous work by Dibblee (1954, 1996), Woodard (1963), Kerr (1982), Winker (1987), Kerr and Kidwell (1991), Winker and Kidwell (1986; 1996), and others. We have analyzed Upper Miocene to lower Pliocene strata exposed in a conformable section in Split Mt. Gorge, including (in order from the base; nomenclature of Winker and Kidwell, 1996): (1) Split Mt. Group: Red Rock Fm alluvial sandstone; Elephant Trees alluvial conglomerate; and lower megabreccia unit; and (2) lower part of Imperial Group, including: Fish Creek Gypsum; proximal to distal turbidites of the Latrania Fm and Wind Caves Mbr of Deguynos Fm; upper megabreccia unit; marine mudstone and rhythmites of the Mud Hills Mbr (Deguynos Fm); and the basal part of the Yuha Mbr (Deguynos Fm). Measured thickness from the base of the Elephant Trees Cgl to the base of the Yuha Mbr is about 1050 m, consistent with previous measurements of Winker (1987). Paleomagnetic samples were collected at approximately 10 m intervals throughout this section. The upper portion of our sampled section overlaps with the lower part of the section sampled for magnetostratigraphic study by Opdyke et al. (1977) and Johnson et al. (1983). They interpreted the base of their section to be about 4.3 Ma, and calculated an average sedimentation rate of approximately 5.5 mm/yr for the lower part of their section. Good-quality preliminary results from 15 paleomagnetic sites distributed throughout our sampled section permit preliminary identification of 6 polarity zones. Based on regional mapping and stratigraphic correlations (Winker and Kidwell, 1996) and extrapolation of the Johnson et al. (1983) sedimentation rates, we tentatively correlate two normal-polarity intervals in the lower part of our section to Chrons C3An.1n and C3An.2n of the geomagnetic polarity time scale of Cande and Kent (1995). If correct, this result would suggest that the lowest reversed-polarity portion of the Red Rock Fm near the base of the section should be correlated to Chron C3Ar.2r, and would be between 6.57 and 6.94 Ma in age. An alternative, but less likely, correlation for the reverse-polarity interval at the base of the section would be with Chron C2Br (7.09-7.43 Ma). This has significant implications for the timing of earliest extension-related basin formation in the western Salton Trough, and potentially raises new questions about the relationship of the Red Rock and Elephant Trees Formations to the Alverson Volcanics (22-14 Ma; Ruisaard, 1979; Kerr, 1982). These preliminary results will be tested and refined with a complete analysis of the remaining samples.