Anatomy of the grainstone shoal facies of the Salem Limestone (Mississippian) of southern Indiana (A preliminary report) (1993)

Item Number: OFS93-03
Price $5.00
Format(s)
Quantity

Authors: J Dodd
Todd Thompson
Daniel Petzold

ABSTRACT: In 1990 M.A. Brown described the middle Mississippian (Valmeyeran) Salem Limestone exposed on the eastern side of the Illinois basin as consisting of a massive grainstone shoal facies behind which developed a sand flat, an open lagoon, and a restricted lagoon facies. The massive shoal facies consists of a series of shoals separated by intershoal areas that connected the lagoon behind the shoal to the open marine environment. Smaller intrashoal channels provided limited exchange between lagoon and open ocean. We have made detailed studies of sedimentary structures and petrography of the shoal facies in three settings: in the shoal proper, in an intrashoal channel, and in an intershoal area. The shoal and intrashoal channel facies consist of tabular-planar and trough cross-stratified beds of grainstone containing echinoderm and fenestrate bryozoan grains as their primary constituents. Ooids increase in abundance toward the top of the section in the intershoal area and intrashoal channel but are not a major constituent except in parts of the intershoal facies. Prominent hardgrounds that have up to 1 m of erosional relief occur in two of the sections. Primary sedimentary features of the shoal facies were produced predominantly by tidal currents and storm reworking of carbonate grains produced in situ and perhaps in part washed in from surrounding environments. Hardgrounds were produced at times of reduced sedimentation rate or possibly during brief periods of subareal exposure. Despite the apparent uniformity of composition of the shoal, porosity and especially permeability varies over a wide range, suggesting a range of cementation patterns within the shoal. Most of the cement in the shoal consists of syntaxial overgrowths on echinoderm grains. Porosity and permeability are greatest in portions of the shoal complex that have not been extensively mechanically and solution packed. Formation of some early meteoric cement probably was the main factor inhibiting compaction. Thick micrite envelopes and oolitic coatings around echinoderms inhibited development of syntaxial cement preventing occlusion of all pore space by later cementation. However, some portions of the intershoal facies that contain a high percentage of ooids have reduced porosity and permeability due to crushing of ooids, producing micrite that clogged the pores. A small amount of the cement in Salem grainstones formed in the marine environment. A larger portion formed by solution of aragonitic grains and reprecipitation as calcite cement. The major portion of the cement probably came from pressure solution, both between grains and along stylolites.



Dodd, J. R., Thompson, T. A., Petzold, D. D. 1993,  Anatomy of the grainstone shoal facies of the Salem Limestone (Mississippian) of southern Indiana (A preliminary report): Indiana Geological Survey Open-File Study 93-03, 51 p., 25 fig.

Notes: Publications in the Indiana Geological Survey Open-File series have been inconsistently named using a variety of series titles including "Open-File Report," "Open-File Map," and "Open-File Study." Prior to 1994, a publication in this series was generally referred to as an "Open-File Report" (but not always). To help reduce confusion created by these inconsistencies, the IGS now refers to every publication in the Open-File series as an "Open-File Study." To be entirely correct in writing a bibliographic reference for a publication, one should use the series name and number that appears on the publication itself.

Appendix.


You may also like:

Keywords: Salem Limestone, Mississippian, shoal, sedimentology, Sanders Group

Can't find what you're looking for? Feel free to contact us directly:

Publication Sales Office
Indiana Geological and Water Survey
611 North Walnut Grove
Bloomington, IN 47405-2208
812-855-7636 (phone)
812-855-2862 (fax)
IGSINFO@indiana.edu

IGS Return Policy

All sales are final. Materials may not be returned after they have been accepted by the customer. Any discrepencies in mail orders must be reported to IGWS within 10 days of receipt of order.

The Indiana Geological and Water Survey will refund the purchase price and sales tax of products if returned with the original sales receipt within 10 days of receipt of order. Refunds will be issued with the same method of payment as indicated on the original receipt except for cash purchases, which will be refunded by check. Items must be returned in the same condition as purchased. Refunds on digital products and services are not allowed, except for defective media such as CD-ROMs, flash drives, and so on. The customer is responsible for paying shipping costs to return items.

Generating Your PDF

Your session for the Indiana Geological and Water Survey will expire in 30 minutes. Please refresh your broswer or click here to restart your session timer.