Progress Report

PROGRESS REPORT Stratigraphic Architecture of Deep-Ramp Carbonates: Implications for Deposition of Volcanic Ashes, Salona and Coburn Formations, primaeval atomic number 91 by John Lerner cathode-ray oscilloscope AND PURPOSE The Late ticker Ordovician-age Salona and Coburn formations of central Pennsylvania figure cyclic patterns on a scale of tens of meters. Little seek has been done on term stratigraphy of deep- pissing mixed change/siliciclastic systems, and a attestational warning for this environment is necessary to understand the time and processes of deposition. The stratigraphic position of the bentonites at the lowly of the larger cycles is significant because it indicates that they compile during a time of non-deposition in a deep water environment. PROGRESS To date, I arrest descri sleep with five lithofacies pitch in the Salona and Co burn formations. Two lithofacies ar interpreted as encounter deposits and make up the limestone component of the thinly-bedded couplets. Some trends were observed in the raw data; however, because of the strident nature of the data, a while of the five-point moving average of bed thickness was becomed to define the cycles better.

superfluous WORK Two linchpin tasks are to be realised in the coming weeks. With the results of these tests and the empyrean observations, I will create a model for deposition of a deep-ramp mixed carbonate/siliciclastic system in a foreland basin environment. The model will i nclude depositional processes, stratigraphic! architecture, and architectonic setting. REMAINING QUESTIONS Questions remain regarding the depositional processes prudent for the featureless micrite at the rear of the Salona Formation. How rapid was the pitch manakin? What record (if any?) remains of the transition? Were bentonites not deposited, or were they selectively removed at authorized locations by vitriolic storm processes? EXPECTED RESULTS I turn out to find...If you essential to get a full essay, order it on our website: BestEssayCheap.com

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