Lithostratigraphy of the Permian Park City Formation Essay
Order ID 53563633773 Type Essay Writer Level Masters Style APA Sources/References 4 Perfect Number of Pages to Order 5-10 Pages Description/Paper Instructions
Task 3 (15 points): Write an article describing the Permian Park City Formation lithostratigraphy. Begin with a paragraph that describes the formation’s regional thickness, aerial occurrence, age, and generalized depositional settings based on regional data. Then, based on your observations in the Limekiln Gulch quarries, describe Lithofacies I, II, III, and IV (from oldest to youngest).
This PP file contains Lithofacies I, II, III, and IV: https://drive.google.com/file/d/1ggYX4-exvFNojISu9
To give you a sense of what to expect for Task 3, here is an example:
An example of the start of a Park City Formation description
The Middle Permian Park City Formation (North American stages: Upper Leonardian/Lower Guadalupian = 275 – 265 Ma) is mostly a fossiliferous micrite deposited on a shallow tropical carbonate shelf. It also has lithologies of dolomite, phosphorite, chert, and quartz sandstone (e.g., class handout). The brachiopod Punctospirifer Pulcher (Stokes, 1988) is a common guide fossil, as are crinoids, bryozoans, rugose corals, and fusulinids. The formation is exposed in thicknesses of up to 600 meters throughout most of northern Utah, northeastern Nevada, southern Idaho, Montana, and Wyoming, as well as western Colorado (http://3dparks.wr.usgs.gov/coloradoplateau/lexicon/parkcity.htm). (This is a link to an external site.)
Within the bottom third of the Park City Formation, exposed in the Limekiln Gulch limestone quarries northwest of the Big U above the University of Utah campus in Salt Lake City, Utah, roughly 30 meters of the stratigraphic section were documented for this study. Based on differing lithofacies, these exposures are classified into four conformable units. Unit I is the oldest and consists of around 5.5 meters of tabular-bedded, medium-gray-weathering biomicrite with bed thicknesses ranging from 20 to 65 centimeters. The lower three meters are mostly detrital micrite, with up to 20% broken brachiopod tests up to one centimeter in length and sparse detrital crinoid stems up to four millimeters in diameter. Up to 10% of bryozoan colonies in growth position are encased in a 25-cm-thick bed in the unit’s center section, with diameters ranging from 0.81.5 cm and lengths ranging from 210 cm. Up to 90% of crinoid stems with diameters of 0.5 to 4 mm, orientated with stem axes perpendicular to bedding, can be found in two identical beds near the top of Unit I. (growth position). In addition, Unit I contains 5% dark gray-weathering dolomite in small lenses and nodules, as well as two 10 mm thick beds (Figure__).
The thickness of Unit II is 13-14 meters, although only the lower 7 meters are accessible for inspection…
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