When examined petrographically the granites of Oklahoma show a marked similarity to the granites of Southeastern Missouri. The same heavy accessory mineral suites are present in the granites of both regions and include: fluorite, zircon, apatite, titanite and epidote. This similarity was further shown by the actual correlation of the heavy mineral suites by types, these types being, based on the heavy mineral distributions of the Missouri Granites
Morphology and internal structures of surface features of the Mare Humorum area were interpreted fro...
Bound typescripts of agents reports, including photographs, charts, clippings, and examples of publi...
Since 1892, the Iowa Geological and Water Survey (IGWS) has provided earth, water, and mapping scien...
In studying the Cut Bank field and its numerous wells, it is found that dry holes are surrounded by ...
During the course of this investigation of the ores of the Big Seven mine, Neihart, Montana, the wri...
Except for the early work of Boutwell and Irving, little has been published on the geology of the Pa...
The Maquoketa Formation (Upper Ordovician-Cincinnatian Series) has been extensively studied for over...
When rainfall occurs that provides more runoff than can be carried within the normal channels of exi...
The Problem. Washington County, Missouri contains a limited number of outcrops of pre-Cambrian igneo...
This investigation was conducted to determine the shrinkage properties of a clay soil whose structur...
Detailed geologic mapping of the Cotter-Jefferson City formational contact in the Thayer, Missouri a...
This study originally was undertaken to describe the witherite identified in specimens collected at ...
This study of the future labor supply and demand in the Omaha area was conducted for the Economic De...
In this pamphlet the process of acculturation among the Dakota Indians--the change which has taken p...
An experimental investigation or the austenite to martensite transformation and the maraging behavio...
Morphology and internal structures of surface features of the Mare Humorum area were interpreted fro...
Bound typescripts of agents reports, including photographs, charts, clippings, and examples of publi...
Since 1892, the Iowa Geological and Water Survey (IGWS) has provided earth, water, and mapping scien...
In studying the Cut Bank field and its numerous wells, it is found that dry holes are surrounded by ...
During the course of this investigation of the ores of the Big Seven mine, Neihart, Montana, the wri...
Except for the early work of Boutwell and Irving, little has been published on the geology of the Pa...
The Maquoketa Formation (Upper Ordovician-Cincinnatian Series) has been extensively studied for over...
When rainfall occurs that provides more runoff than can be carried within the normal channels of exi...
The Problem. Washington County, Missouri contains a limited number of outcrops of pre-Cambrian igneo...
This investigation was conducted to determine the shrinkage properties of a clay soil whose structur...
Detailed geologic mapping of the Cotter-Jefferson City formational contact in the Thayer, Missouri a...
This study originally was undertaken to describe the witherite identified in specimens collected at ...
This study of the future labor supply and demand in the Omaha area was conducted for the Economic De...
In this pamphlet the process of acculturation among the Dakota Indians--the change which has taken p...
An experimental investigation or the austenite to martensite transformation and the maraging behavio...
Morphology and internal structures of surface features of the Mare Humorum area were interpreted fro...
Bound typescripts of agents reports, including photographs, charts, clippings, and examples of publi...
Since 1892, the Iowa Geological and Water Survey (IGWS) has provided earth, water, and mapping scien...