Origin of mass flow sedimentary structures in hemipelagic basin deposits: Santa Barbara Basin,California Borderland |
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Authors: | Scott E Thornton |
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Institution: | (1) Unocal International, Box 7600, 90051 Los Angeles, CA |
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Abstract: | Holocene mass flow processes produce distinctive sedimentary structures in this silled, anoxic basin characterized by high
sedimentation rates of fine-grained fill. Mud flow deposits possess a 0899 1444 V
3 diagnostic vertical sequence of structures on the lower slope. Basin floor turbidites possess a variety of bed set combinations
of: 1) finely laminated layers, 2) graded silt and clay layers, and 3) ungraded, massive silts and clays with floating sand
grains. Massive, ungraded flood-derived suspensate deposits can be distinguished from turbidites. Turbidites and suspensate
deposits constitute 30% of the sampled sediment column. Varve counting of the remaining 70% provides frequencies of turbidite
and flood suspensate layer deposition. |
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Keywords: | |
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