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Group showing the varied use of Indiana Limestone, 1920.

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Front cover of Indiana Limestone: The Aristocrat of Building Materials, 1920

"Indiana Limestone used as a veneer for walls of stud frame construction, brick, or hollow tile is fast becoming popular among builders of small homes and bungalows. Short-length stock of about 4" thickness laid up as a random ashlar is the most economical form of stone construction. It is also thoroughly practical and highly pleasing in its effect. "Cut stone contractors who keep a large supply of this stock on hand will find it highly profitable, as the demand for it among architects and builders is rapidly increasing. "Our handsomely illustrated booklet, 'Indiana Limestone for School and College Buildings,' showing various interesting uses of the stone will be sent free upon request.

4-The age of the Chaqchaq limestone is late Maastrichtian.

Front cover of Indiana Limestone: The Aristocrat of Building Materials, 1920

The upper and lower Bakken members are similar in that they are hard, siliceous, pyritic, fissile, brownish black to dark black, often noncalcareous, and organic-rich shales. The shales are very uniform throughout their extents; however, some cores of the lower shale have thin (3 feet) black limestone that is coarsely crystalline and significantly lower in organic content.

Lithofacies 5 – SILTSTONE, massive, dense, mottled, dolomite, argillaceous, tan to light gray, fossiliferous, disseminated pyrite, slightly bioturbated; contact with upper member is sharp. Cross-ripple laminations, as much as 6 inches thick, occur lower in half of section (occasionally fossiliferous).

Lithofacies 4 – LOWER ARGILACEOUS PACKSTONE TO FINE-GRAINED SANDSTONE AND UPPER INTERBEDS OF DARK GRAY SHALE AND BUFF SILTY SANDSTONE. Lower portion is medium gray, very fine-grained, dolomite cement, with thin parallel laminations. Upper portion is thinly laminated to cross-bedded siltstones and very fine grained sandstones, with moderately bioturbated, vertical burrows. Dolomitic cement in upper and lower portions with some dewatering structures.

Lithofacies 3 – DARK GRAY, FINE-GRAINED SANDSTONE TO MEDIUM-GRAY LIMESTONE. Sandstone is mainly quartzose with minor feldspar and heavy minerals, buff to green, moderately well sorted to well-sorted, rounded to well-rounded, contains calcite cement with occasional pyritic cement, disseminated pyrite, few brachiopods, and slight to no bioturbation. Limestone occurs along the southwestern extent and ranges from sand–algal packstone, to ooid packstone, to an ooid–crinoid packstone–grainstone. Oil staining may be present in the very fine grained, laminated, predominantly quartz sandstone portion.

Lithofacies 2 – GREENISH GRAY ARGILLACEOUS SILTSTONE TO BROWNISH GRAY SILTY SANDSTONE. Siltstone is moderately to very strongly bioturbated (disrupting the laminae), fossiliferous, dolomitic becoming calcareous with depth, and disseminated pyrite. Sandstone accumulations are restricted to localized highs.

Lithofacies 1 – ARGILLACEOUS SILTSTONE, massive, dense, mottled, very calcareous, gray-green, highly fossiliferous, with disseminated pyrite. The lower contact may be either gradational or erosive.

More than 50 percent of the surface rocks in Kentucky are limestones

Limestone, a principle ore of calcuim contains 76.14% Ca by mass. How many of Ca can be obtained from 4.18X10^2hg of the ore?

“Soldiers’ Memorial Monument of No. 1 Buff Indiana Limestone in Yard of the St. James Church, Toronto, Ontario. Architects: Sproatt & Rolph. Stone furnished by Indiana Quarries Company.”

According to Ozcan (2007) [12], the occurrence of Omphalocyclus in different stratigraphic levels, ranging in age from Campanian to late Maastrichtian in Turkey is documented. The genus is quite rare in the (late) Campanian, becoming more frequent in late Campanian early Maastrichtian and late Maastrichtian beds. Enos et al (1995) [13] found this fauna in the Maastrichtian rocks of Marshall Islands and considered it as Maastrichtian index. Omphalocyclus is benthic foraminifera, known from the relatively shallow-water paleoenvironment located in the outer parts of the Late Cretaceous Tethyan platforms. The mineralogy of this type of the forams is calcitic by which the shell microstructure is well preserved which similar to Orbitoid but with larger and discoidal shape instead of fusiform. It is common in both Chaqchaq limestone and Aqra Formation at Chwarta-Mawat area (Fig.6A).

Conservation of the endangered limestone endemic ; effects of anthropogenic disturbance on habitat and life history.
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LIMESTONE COUNTY | The Handbook of Texas Online| …

"Despite the misleading name, the Exhibition is actually a permanent museum. It documents the development of the local dimension stone industry from 1850 to 1910. These exhibits include quarrying and milling operations from the early-1900s to the present. A photographic exhibit documents buildings constructed of Bedford limestone. Other exhibits include local geology, fossils, and the artistic use of limestone in memorials and otherwise."

The Upper Jurassic reservoirs consist mainly of limestone.

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Thesis Of Limestone – 211677 – SMK Muhammadiyah 2 …

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Synthesis of Precipitated Calcium Carbonate Using a Limestone ..

Origin of Fossiliferous Limestone Beds inside the Upper Part of Tanjero Formation at the Northwest of Sulaimani Area, Kurdistan Region, NE-Iraq

Lithology | Bakken - Beyond the Boom

Statistical downscaling of temperature and precipitation for climate change impact assessment of rare plants on the limestone barrens of Northwestern Newfoundland.

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