About 30ft. of the lower section of core. Black and red lines help keep orientation of the pieces. The white rock is a lime-stone that quickly changes to a darker shale. A piece from the upper section of the core. The lithology is shale. Lamination of coarser material is silt. The dark lamination contain a variety of shells. The ellipses are compressed burrows formed by ancient sea creatures. dot on thin section B. On the right of the picture a brachiopod is pressed against a bryozoan signify-to the silty material to the left of the shell. Sedimentology of the “Utica ” below Cinncinat
The “butter shale” Lagerstätten of the Cincinnati Arch have produced an abundance of articulated tri...
Sedimentological and biostratigraphic investigations of 15 cores (total length: 88 m) from the vicin...
Limestones and shales of the Grant Lake Formation (Upper Ordovician; Katian; Maysvillian) are well e...
Subsurface geology can be directly observed by means of vertical cores taken at a study site. Invest...
The Manchester edrioasteroid pavement is a shell layer in mudrock from the Corryville Formation (U. ...
ABSTRACT: A unique carbonate bed occurs within the dominantly siliciclastic Catskill Magnafaeies (Up...
A series of cores drilled to a depth of ~400 ft from lower Kope Fm. (mid Katian) downward to the Hig...
A distinct sequence of orange-brown, fossiliferous grainstones with interbedded blue mudstones exist...
The photomicrographs and other illustrations on this website accompany interpretations by the author...
The mechanical stratigraphy of the Upper Ordovician Utica Shale is characterized by studying outcrop...
<p>A. Bioturbated ripple laminated silt-claystone. (<i>Planolites</i> marked by black arrows and <i>...
A quantitative study is made of the organic and inorganic onstituents of a sequence of Devonian lime...
Oriented rectangular cores of 20.3 × 30.5 cm and 45.7 cm high have been collected in a number of sub...
The largest and most extensive, known, Early Llandovery (Rhuddanian) biohermal complex is exposed wi...
Analysis of the fabric of laminated black mudstones of the Ore-Bearing Częstochowa Clay Formation (B...
The “butter shale” Lagerstätten of the Cincinnati Arch have produced an abundance of articulated tri...
Sedimentological and biostratigraphic investigations of 15 cores (total length: 88 m) from the vicin...
Limestones and shales of the Grant Lake Formation (Upper Ordovician; Katian; Maysvillian) are well e...
Subsurface geology can be directly observed by means of vertical cores taken at a study site. Invest...
The Manchester edrioasteroid pavement is a shell layer in mudrock from the Corryville Formation (U. ...
ABSTRACT: A unique carbonate bed occurs within the dominantly siliciclastic Catskill Magnafaeies (Up...
A series of cores drilled to a depth of ~400 ft from lower Kope Fm. (mid Katian) downward to the Hig...
A distinct sequence of orange-brown, fossiliferous grainstones with interbedded blue mudstones exist...
The photomicrographs and other illustrations on this website accompany interpretations by the author...
The mechanical stratigraphy of the Upper Ordovician Utica Shale is characterized by studying outcrop...
<p>A. Bioturbated ripple laminated silt-claystone. (<i>Planolites</i> marked by black arrows and <i>...
A quantitative study is made of the organic and inorganic onstituents of a sequence of Devonian lime...
Oriented rectangular cores of 20.3 × 30.5 cm and 45.7 cm high have been collected in a number of sub...
The largest and most extensive, known, Early Llandovery (Rhuddanian) biohermal complex is exposed wi...
Analysis of the fabric of laminated black mudstones of the Ore-Bearing Częstochowa Clay Formation (B...
The “butter shale” Lagerstätten of the Cincinnati Arch have produced an abundance of articulated tri...
Sedimentological and biostratigraphic investigations of 15 cores (total length: 88 m) from the vicin...
Limestones and shales of the Grant Lake Formation (Upper Ordovician; Katian; Maysvillian) are well e...