Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Uranium in the Carnmenellis granite, Cornwall, England

Technical Report ·
OSTI ID:5129164
Samples from a 30 meter core from the Rosemanowas quarry in the Carnmenellis granite in Cornwall, England were analyzed by induced fission track detection, delayed neutron detection, backscattered electron imaging in a SEM, and energy dispersive x-ray spectrometry. Uranium occurs mainly in: (1) primary accessory minerals; (2) alteration and replacement phases, and (3) microcrack-sealing phases. Zircon, monazite, and apatite are common uraniferous primary accessory minerals. Uraniferous alteration phases include hematite, rutile and pyrolusite. Hematite is a common uraniferous replacement phase. Most sealed microcracks contain uranium. Hematite and pyrolusite are ubiquitous uraniferous crack-sealing phases. Autunite and churchite are occasional uraniferous crack-sealing phases. Whole rock uranium concentrations are extremely variable. High uranium contents result from high percentages of uraniferous primary accessory phases and/or rutile. Hydrothermal activity, such as hematization, can result in depleted whole rock uranium concentrations. Results of this study indicate that uranium and light rare earth elements have been mobilized and redistributed in this section of the Carnmenellis granite by postmagmatic processes. 28 refs., 13 figs. 2 tabs.
Research Organization:
Wellesley Coll., MA (USA). Dept. of Geology
DOE Contract Number:
AC02-78ER04972
OSTI ID:
5129164
Report Number(s):
DOE/ER/04972-T3; ON: DE86000879
Country of Publication:
United States
Language:
English

Similar Records

Microcracks and energy. Progress report, 1 March 1982-28 February 1983
Technical Report · Mon Feb 28 23:00:00 EST 1983 · OSTI ID:6349092

Uraniferous accessory phases in granites
Conference · Mon Dec 31 23:00:00 EST 1984 · Geol. Soc. Am., Abstr. Programs; (United States) · OSTI ID:6202556

Uraniferous microcracks in granites
Conference · Mon Dec 31 23:00:00 EST 1984 · Geol. Soc. Am., Abstr. Programs; (United States) · OSTI ID:6677613