Sedimentation across the central California oxygen minimum zone: an alternative coastal upwelling sequence.
Journal of Sedimentary Petrology
By: T. L. Vercoutere, H.T. Mullins, K. McDougall, and J.B. Thompson
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Abstract
Distribution, abundance, and diversity of terrigenous, authigenous, and biogenous material provide evidence of the effect of bottom currents and oxygen minimum zone (OMZ) on continental slope sedimentation offshore central California. Three major OMZ facies are identified, along the upper and lower edges of OMZ and one at its core.-from Authors
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Sedimentation across the central California oxygen minimum zone: an alternative coastal upwelling sequence. |
| Series title | Journal of Sedimentary Petrology |
| Volume | 57 |
| Issue | 4 |
| Year Published | 1987 |
| Language | English |
| Larger Work Type | Article |
| Larger Work Subtype | Journal Article |
| Larger Work Title | Journal of Sedimentary Petrology |
| First page | 709 |
| Last page | 722 |
| Google Analytic Metrics | Metrics page |