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Full-Text Articles in Physical Sciences and Mathematics
Petrology Of The Farmington Gabbro-Metagabbro Complex, North Carolina, James Thomas Harden
Petrology Of The Farmington Gabbro-Metagabbro Complex, North Carolina, James Thomas Harden
Masters Theses
The Farmington gabbro-metagabbro complex is located along the western margin of the Charlotte belt of North Carolina. At least twp or more intrusions occur within the complex. The Farmington gabbroic intrusion is postmetamorphic and contains plagioclase, hornblende, orthopyroxene, clinopyroxene, and olivine. Small amounts of magnetite, ilmenite, pyrite, pyrrhotite, pentlandite, hematite, hercynitic spinel, and biotite occur. Textures are hypidiomorphic granular to hypidiomorphic inequigranular. Four types of gabbroic rocks are present; hornblende gabbronite, olivine-hornblende gabbronorite, hornblende norite, and olivine-hornblende norite, with olivine-hornblende gabbronorite predominating. A limited range of progressive differentiation is indicated by restricted increases in FeO/(FeO +MgO) ratios for mafic silicates …
Late Quaternary Vegetational History At Cupola Pond, Ozark National Scenic Riverways, Southeastern Missouri, Everett Newman Smith Jr.
Late Quaternary Vegetational History At Cupola Pond, Ozark National Scenic Riverways, Southeastern Missouri, Everett Newman Smith Jr.
Masters Theses
A 12 meter core of lacustrine sediments from Cupola Pond, Ripley County, Missouri, Provides the first continuous record in the Ozark Plateaus Region of ecologic changes from full-glacial time to the present. From 17,100 to 15,350 yr B.P., forest communities were dominated by jack and/or red pine (northern Diploxylon Pinus) and spruce (Picea). A late-glacial, transitional forest of oak (Quercus), ash (Fraxinus), pine and spruce characterized the upland vegetation that occurred during a period of climatic amelioration between 15,350 and 12,300 yr B.P. The early Holocene period from 12,300 to 9,100 yr B.P. …