Penrose Conference SUBDUCTION TO STRIKE-SLIP TRANSITIONS ON PLATE BOUNDARIES Puerto Plata, Dominican Republic January 18-24, 1999 ABSTRACT VOLUME Conveners: Paul Mann, Nancy Grindlay and James Dolan Sponsored by the Geological Society of America, Petroleum Research Fund, NSF and NASA Penrose Conference: Subduction to Strike-Slip Transitions on Plate Boundaries, Jan. 18-24, 1999 STRUCTURAL GEOLOGY AND SEDIMENTOLOGY OF A PLIOCENE INNER-TRENCH SLOPE SUCCESSION, NORTHWESTERN ECUADOR K. R. AALTO Dept. of Geology, Humboldt State Univ., Arcata, CA, USA 95521,
[email protected] The Pliocene Upper Onzole Formation exposed in the vicinity of Punta Gorda, near Esmeraldas, Ecuador, is composed mainly of fine-grained mud turbidites, having regular vertical sequences of sedimentary structures associated with a positive grading, and bioturbation restricted mostly to the tops of beds. The remainder of beds measured consist of volcanic ash, mud pelagite, and glauconitic silt-sand turbidites. Vertical sequential analysis of stratigraphic sections for the most part show no pronounced trends in bed thickness or grain size. Volcanic ashes are crystal-vitric tuffs occurring in four bedding styles: A) normally- graded ashes with burrowed gradational tops and sharp wavy bases; B) ashes that form part of a complex microstratigraphy consisting of thinly-bedded mudstone, silt-sand turbidites, tuffaceous mudstone, and ash beds; C) less conspicuous ash laminae and ash-filled burrows; and D) a tuffaceous bed with ash and mud swirled together in convolute layers. Ash chemistry suggests an Andean high-K calc-alkaline provenance. Facies relations, paleontologic data and regional geologic setting suggest sediment accumulation on an inner trench slope in a basin situated oceanward of the Pliocene trench-slope break.