TRIASSIC PHOSPHATIC ROCKS OF NORTHERN ALASKA: SPATIAL AND TEMPORAL DEPOSITIONAL PATTERNS ON A HIGH-LATITUDE, LOW-ANGLE RAMP
Ladinian HPS constitute a petrographically distinct interval up to 7 m thick recognized across 80 km of outcrop in the NE Brooks Range and in several wells 110 km to the NW. Beds are parallel- and cross-laminated and contain transported, sand-sized phosphatic clasts—mainly simple peloids and phosphate-coated quartz grains and flat clam fragments—cemented by silica, phosphate, and/or calcite. Phosphate content and grain packing decrease upward within the interval and carbonate content increases. These strata formed on the middle ramp during transgressive and early regressive parts of a 2nd or 3rd order depositional cycle.
Norian HPS are more widely distributed and heterogeneous than those of Ladinian age. The Norian HPS occur through a ~80 by 180 km outcrop area, and in numerous wells on the eastern North Slope. Phosphate in these strata is both transported and in situ and is chiefly cm-scale nodules and sand-sized peloids. It is most abundant in intervals ≤ 2 m thick at the tops of regressive limestone parasequences that were deposited on the middle to inner ramp.
HPS of other ages are less common. Smithian-Anisian HPS include phosphate ± chert clast conglomerates in a few west and central N Slope wells and phosphatic nodule horizons that top siltstone parasequences in some Brooks Range outcrops. Carnian HPS that contain concentrations of phosphatic nodules and peloids occur mainly in 2 N Slope wells.
The Shublik Fm. represents part of a worldwide shift of phosphorite formation into higher latitudes during the Triassic. If, as previously suggested, HPS in the Shublik formed in response to a marine upwelling system, our data show that the effects of this system varied through space and time.