Nature of the southwestern boundary of the central Mojave Tertiary province, Rodman Mountains, California

Tertiary volcanic and sedimentary rocks in the central Mojave Desert are la rgely confined to the Barstow-Bristol trough, an elongate tectonic depressi on filled with lower Miocene strata, The southwestern boundary of the troug h is sharply defined and separates thick (>2 km) Tertiary sequences from an area to the southwest that is virtually devoid of Tertiary rocks. Segments of this boundary have been interpreted as a buttress unconformity, as a ri ght-slip sidewall fault that formed the lateral boundary of an early Miocen e extensional terrane, and as a dip-slip fault caused by flexure of the Nor th American plate above the subducted Mendocino fracture zone. The Silver B ell fault in the Rodman Mountains, central Mojave Desert, is the best expos ed segment of the boundary, and relations exposed along it can be used to t est these hypotheses. The Tertiary sequence north of the Silver Bell fault is at least 2.3 km thi ck and comprises at least 1.9 km of mafic lava flows overlain by and interc alated with coarse elastic rocks derived from the south side of the fault. Stratigraphic relations require faulting during volcanism and indicate that the minimum throw across the fault is at least equal to the thickness of t he exposed Tertiary section. Tuff layers intercalated in the lower part of the elastic deposits are 23-24 m.y. old, indicating that faulting and volca nism were contemporaneous with extension and plutonism in the nearby centra l Mojave metamorphic core complex. Structural and stratigraphic data indica te that the Silver Bell fault is primarily a dip-slip fault. The Tertiary section is folded into a west-trending, upright to overturned syncline located near the southern edge of exposed Tertiary rocks. The sync line records late Cenozoic north-south shortening along the northwest-strik ing Calico fault, which in this area accommodated about 10 km of right slip and perhaps 1 km of reverse slip. Southwestward-dipping strata in the area lly extensive north limb of the syncline resemble tilted strata in nearby h ighly extended areas and have been interpreted to reflect crustal extension , However, bedding dip does not decrease upward in the Tertiary section, pa leocurrent directions trend obliquely updip, and northeast-dipping normal f aults are rare. Stratal tilting postdated the accumulation of the exposed s ection, which therefore was not deposited during rotational normal faulting . The new data contradict interpretation of the Silver Bell fault as a major right-slip fault bounding the central Mojave extensional terrane, although they permit small-magnitude extension across the fault. The amount of early Miocene crustal extension in this area therefore is apparently small in sp ite of stratal tilting, and the lateral limit of large-magnitude crustal ex tension in the central Mojave block is farther northwest, The data are cons istent with the fault having formed by failure during plate flexure above t he subducted Mendocino fracture zone.