The petrology and geochemistry of the Arbuckle Group have been neglected recently, especially in light of the wealth of new information on carbonates and the tectonic history of the area. This study deals with the Ordovician Butterly Dolomite, one of seven formations of the Arbuckle Group in the Arbuckle Mountain area.Geolog
Sphalerite in the Arbuckle dolomite of Western Kansas was described by the writer in 1948 (1). Conti...
Dolomites within the Lower Ordovician Ellenburger Group can be broadly subdivided into two groups, t...
Replacement dolomite occurs in Jurassic Samanasuk Formation in Dara Adam khel area of Kohat ranges, ...
The Mascot-Jefferson City (MJC) district of East Tennessee is the largest of several Appalachian-sty...
The Arbuckle Group has a gross thickness in excess of 10,000 feet in the southern Oklahoma aulacogen...
The Mascot Dolomite, the upper unit of the Cambrian-Ordovician Knox Group, is a major host for Missi...
Regional geological studies in southeastern Missouri have made a significant contribution to knowled...
Cambrian-Ordovician age Arbuckle Group carbonates host a wide variety of petroleum, mineral, and fre...
The carbonates of the Mississippian Pahasapa Limestone in the northeastern sector of the Black Hills...
The formation of the southeast Missouri Mississippi Valley-type Pb, Zn, Cu ore districts have been a...
Author Institution: Department of Geology, Miami UniversityThe Devonian rocks at Pugh Quarry have th...
Author Institution: Department of Geology, Miami UniversityCalcite is by far the most abundant miner...
The Gasconade Formation (Lower Ordovician) has been studied in the surface and subsurface in the Oza...
This study concerns itself with several suites of freshwater carbonates which are representative of ...
Cambrian-Ordovician Arbuckle Group rocks in Kansas occur entirely in the subsurface. As is demonstra...
Sphalerite in the Arbuckle dolomite of Western Kansas was described by the writer in 1948 (1). Conti...
Dolomites within the Lower Ordovician Ellenburger Group can be broadly subdivided into two groups, t...
Replacement dolomite occurs in Jurassic Samanasuk Formation in Dara Adam khel area of Kohat ranges, ...
The Mascot-Jefferson City (MJC) district of East Tennessee is the largest of several Appalachian-sty...
The Arbuckle Group has a gross thickness in excess of 10,000 feet in the southern Oklahoma aulacogen...
The Mascot Dolomite, the upper unit of the Cambrian-Ordovician Knox Group, is a major host for Missi...
Regional geological studies in southeastern Missouri have made a significant contribution to knowled...
Cambrian-Ordovician age Arbuckle Group carbonates host a wide variety of petroleum, mineral, and fre...
The carbonates of the Mississippian Pahasapa Limestone in the northeastern sector of the Black Hills...
The formation of the southeast Missouri Mississippi Valley-type Pb, Zn, Cu ore districts have been a...
Author Institution: Department of Geology, Miami UniversityThe Devonian rocks at Pugh Quarry have th...
Author Institution: Department of Geology, Miami UniversityCalcite is by far the most abundant miner...
The Gasconade Formation (Lower Ordovician) has been studied in the surface and subsurface in the Oza...
This study concerns itself with several suites of freshwater carbonates which are representative of ...
Cambrian-Ordovician Arbuckle Group rocks in Kansas occur entirely in the subsurface. As is demonstra...
Sphalerite in the Arbuckle dolomite of Western Kansas was described by the writer in 1948 (1). Conti...
Dolomites within the Lower Ordovician Ellenburger Group can be broadly subdivided into two groups, t...
Replacement dolomite occurs in Jurassic Samanasuk Formation in Dara Adam khel area of Kohat ranges, ...