Add to ORKGThe Toronto cyclothem is the lower limestone member of the Oread megacyclothem of the Shawnee group, Virgilian series, Pennsylvanian system and crops of in a linear belt extending north-south for a distance of 300 miles across Oklahoma, Kansas, and parts of Missouri and Nebraska
A stratigraphic study of the plant microfossils m the Iowa Pennsylvanian coals by the maceration met...
The Mississippian system confined to the subsurface between depths of 7,100 and 12,650 feet is compo...
As in Kansas where distinct zonation of corals has been recognized, the dissepimental Rugosa Dibunop...
major marine cyclothems, each consisting of a thin transgressive limestone, thin offshore dark phosp...
The Shawnee Group extends from Oklahoma through Kansas, Missouri, Iowa, and Nebraska. In Oklahoma mu...
Includes bibliographical references (p. 70-71).Introduction -- Previous investigations -- Preparatio...
The Fort Hays Limestone is upper Cretaceous (Coniacian) in age and occurs in a wide area across the ...
A thin (3-25 cm), persistent conglomerate-sandstone unit occurs at the base of the transgressive sys...
The Middle and Late Pennsylvanian succession of Kansas consists of two types of cyclothems, litholog...
The rocks of the lower part of the Council Grove Group (“Early Permian”) have been examined along th...
Ten cyclothems from the Wolfcampian of northeastern Kansas, including parts of the Council Grove and...
The nature and lateral variation of a host rock limestone in the Tri-State zinc-lead district were p...
The Upper Pennsylvanian (Missourian) Lansing-Kansas City Group of eastern, southcentral and western ...
In southeastern Kansas, the Middle Pennsylvanian (Desmoinesian) Bandera Shale consists of sandstone,...
In southeastern Kansas, the Middle Pennsylvanian (Desmoinesian) Bandera Shale consists of sandstone,...
A stratigraphic study of the plant microfossils m the Iowa Pennsylvanian coals by the maceration met...
The Mississippian system confined to the subsurface between depths of 7,100 and 12,650 feet is compo...
As in Kansas where distinct zonation of corals has been recognized, the dissepimental Rugosa Dibunop...
major marine cyclothems, each consisting of a thin transgressive limestone, thin offshore dark phosp...
The Shawnee Group extends from Oklahoma through Kansas, Missouri, Iowa, and Nebraska. In Oklahoma mu...
Includes bibliographical references (p. 70-71).Introduction -- Previous investigations -- Preparatio...
The Fort Hays Limestone is upper Cretaceous (Coniacian) in age and occurs in a wide area across the ...
A thin (3-25 cm), persistent conglomerate-sandstone unit occurs at the base of the transgressive sys...
The Middle and Late Pennsylvanian succession of Kansas consists of two types of cyclothems, litholog...
The rocks of the lower part of the Council Grove Group (“Early Permian”) have been examined along th...
Ten cyclothems from the Wolfcampian of northeastern Kansas, including parts of the Council Grove and...
The nature and lateral variation of a host rock limestone in the Tri-State zinc-lead district were p...
The Upper Pennsylvanian (Missourian) Lansing-Kansas City Group of eastern, southcentral and western ...
In southeastern Kansas, the Middle Pennsylvanian (Desmoinesian) Bandera Shale consists of sandstone,...
In southeastern Kansas, the Middle Pennsylvanian (Desmoinesian) Bandera Shale consists of sandstone,...
A stratigraphic study of the plant microfossils m the Iowa Pennsylvanian coals by the maceration met...
The Mississippian system confined to the subsurface between depths of 7,100 and 12,650 feet is compo...
As in Kansas where distinct zonation of corals has been recognized, the dissepimental Rugosa Dibunop...
