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Facies architecture of Tocito Shelf sandstone, Northwest New Mexico

Conference ·
OSTI ID:6921054

Outcrops along the northwest margin of the San Juan basin reveal a Tocito sandstone ridge complex that overlies a transgressive surface. The ridge complex contains laterally extensive pebble lags that traverse facies boundaries. These lags distinguish three stages of ridge growth interrupted by two erosional hiatuses. During stage one, bioturbated muddy fine sandstone, thin ripple-bedded sandstone, and sandy mudstone were deposited. In stage two, bioturbated muddy sandstone interfingered with interbedded muddy sandstone and sandy mudstone capped by cross-bedded sandstone. In stage three, cross-bedded sandstone with rare basal bioturbated muddy sandstone was deposited. Collectively, these deposits compose an upward-shoaling sequence inferred to have formed apt ''paracycle'' stillstand of the Coniacian transgression. Exposures of strata below the transgressive surface and subsurface data from Bisti oil field reveal evidence for earliest Coniacian(.) relative sea level prior to ''Tocito'' transgression. In outcrop, this fall is expressed by incision of fine-grained Gallup ''A'' tongue shoreface sandstone by coarser Torrivio fluvial sandstone. Downdip at Bisti field, examination of well cores linked to over 200 electric logs revealed a terraced shelf topography. An upward increase in maximum and median grain size across this terraced surface is inferred to result from the distribution of coarse Torrivio sediments distributed onto the shelf at low-stand. These shelf at sediments are inferred to be the source for the sandstone ridges at Bisti field. Integral sandstone ridges (2.5 km/sup 2/) are en echelon with an across-ridge spacing of 1,500 m between crests, and form a linear sandstone ridge complex (250 km/sup 2/) on isopach maps of crossbedded sandstone facies.

OSTI ID:
6921054
Report Number(s):
CONF-880301-
Country of Publication:
United States
Language:
English

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