Microcrack technology. Progress report, 1 April 1979-29 February 1980
Microcracks in samples of core from a 3000-foot hole in the Conway granite, near North Conway, New Hampshire, are abundant and most of them are sealed with siderite, chlorite, quartz, hematite, clay, or microbreccia. The sealed cracks are 1 to 100.mu. wide, intersect many grain boundaries, often coi...
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Massachusetts Institute of Technology. Department of Earth and Planetary Sciences.
1980
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ftunivnotexas:info:ark/67531/metadc1090417 2023-05-15T17:35:21+02:00 Microcrack technology. Progress report, 1 April 1979-29 February 1980 Simmons, G. Caruso, L. Padovani, E. 1980-03-01 62 pages Text https://doi.org/10.2172/5697427 https://digital.library.unt.edu/ark:/67531/metadc1090417/ English eng Massachusetts Institute of Technology. Department of Earth and Planetary Sciences. rep-no: DOE/ER/04972-2 grantno: AC02-78ER04972 doi:10.2172/5697427 osti: 5697427 https://digital.library.unt.edu/ark:/67531/metadc1090417/ ark: ark:/67531/metadc1090417 Granites Thorium Chlorite Minerals Rocks Iron Carbonates Iron Ores Quartz Oxides Water Shales 54 Environmental Sciences Carbonates Hematite North Atlantic Region Minerals Siderite Cracks Chalcogenides Gamma Spectroscopy Transition Element Compounds Radionuclide Migration Clays 58 Geosciences Data Carbon Compounds 12 Management Of Radioactive And Non-Radioactive Wastes From Nuclear Facilities Iron Oxides Ores Mass Transfer Sedimentary Rocks Carbon Oxides Actinides Silicon Compounds Spectroscopy Silicon Oxides Metals Elements New Hampshire Data Compilation Images Igneous Rocks Environmental Transport 580300 -- Mineralogy Petrology & Rock Mechanics-- (-1989) Oxygen Compounds Tables Numerical Data Uranium Information Report 1980 ftunivnotexas https://doi.org/10.2172/5697427 2022-08-27T22:08:03Z Microcracks in samples of core from a 3000-foot hole in the Conway granite, near North Conway, New Hampshire, are abundant and most of them are sealed with siderite, chlorite, quartz, hematite, clay, or microbreccia. The sealed cracks are 1 to 100.mu. wide, intersect many grain boundaries, often coincide with grain boundaries, and both intersect and contain minerals that are normally rich in U and Th. The abundances of U and Th in 100-gm-bulk samples range from 0.1 to 30 ppM and from 6 to 100 ppM, respectively. The working hypothesis that U and Th have migrated through the microcracks in CO/sub 2/-rich waters is proposed. In the Redstone Quarry core, the presently open microcracks are preferentially oriented; most open cracks have horizontal surfaces. Samples of Devonian shales have been obtained for the purpose of examining microcracks in relation to the production of natural gas. The problems of sample preparation for fissile shale have been largely solved. Samples from the NTS have been prepared for the examination of microcracks in relation to possible disposal sites for radioactive waste. Report North Atlantic University of North Texas: UNT Digital Library Conway ENVELOPE(-61.422,-61.422,-62.841,-62.841) |
institution |
Open Polar |
collection |
University of North Texas: UNT Digital Library |
op_collection_id |
ftunivnotexas |
language |
English |
topic |
Granites Thorium Chlorite Minerals Rocks Iron Carbonates Iron Ores Quartz Oxides Water Shales 54 Environmental Sciences Carbonates Hematite North Atlantic Region Minerals Siderite Cracks Chalcogenides Gamma Spectroscopy Transition Element Compounds Radionuclide Migration Clays 58 Geosciences Data Carbon Compounds 12 Management Of Radioactive And Non-Radioactive Wastes From Nuclear Facilities Iron Oxides Ores Mass Transfer Sedimentary Rocks Carbon Oxides Actinides Silicon Compounds Spectroscopy Silicon Oxides Metals Elements New Hampshire Data Compilation Images Igneous Rocks Environmental Transport 580300 -- Mineralogy Petrology & Rock Mechanics-- (-1989) Oxygen Compounds Tables Numerical Data Uranium Information |
spellingShingle |
Granites Thorium Chlorite Minerals Rocks Iron Carbonates Iron Ores Quartz Oxides Water Shales 54 Environmental Sciences Carbonates Hematite North Atlantic Region Minerals Siderite Cracks Chalcogenides Gamma Spectroscopy Transition Element Compounds Radionuclide Migration Clays 58 Geosciences Data Carbon Compounds 12 Management Of Radioactive And Non-Radioactive Wastes From Nuclear Facilities Iron Oxides Ores Mass Transfer Sedimentary Rocks Carbon Oxides Actinides Silicon Compounds Spectroscopy Silicon Oxides Metals Elements New Hampshire Data Compilation Images Igneous Rocks Environmental Transport 580300 -- Mineralogy Petrology & Rock Mechanics-- (-1989) Oxygen Compounds Tables Numerical Data Uranium Information Simmons, G. Caruso, L. Padovani, E. Microcrack technology. Progress report, 1 April 1979-29 February 1980 |
topic_facet |
Granites Thorium Chlorite Minerals Rocks Iron Carbonates Iron Ores Quartz Oxides Water Shales 54 Environmental Sciences Carbonates Hematite North Atlantic Region Minerals Siderite Cracks Chalcogenides Gamma Spectroscopy Transition Element Compounds Radionuclide Migration Clays 58 Geosciences Data Carbon Compounds 12 Management Of Radioactive And Non-Radioactive Wastes From Nuclear Facilities Iron Oxides Ores Mass Transfer Sedimentary Rocks Carbon Oxides Actinides Silicon Compounds Spectroscopy Silicon Oxides Metals Elements New Hampshire Data Compilation Images Igneous Rocks Environmental Transport 580300 -- Mineralogy Petrology & Rock Mechanics-- (-1989) Oxygen Compounds Tables Numerical Data Uranium Information |
description |
Microcracks in samples of core from a 3000-foot hole in the Conway granite, near North Conway, New Hampshire, are abundant and most of them are sealed with siderite, chlorite, quartz, hematite, clay, or microbreccia. The sealed cracks are 1 to 100.mu. wide, intersect many grain boundaries, often coincide with grain boundaries, and both intersect and contain minerals that are normally rich in U and Th. The abundances of U and Th in 100-gm-bulk samples range from 0.1 to 30 ppM and from 6 to 100 ppM, respectively. The working hypothesis that U and Th have migrated through the microcracks in CO/sub 2/-rich waters is proposed. In the Redstone Quarry core, the presently open microcracks are preferentially oriented; most open cracks have horizontal surfaces. Samples of Devonian shales have been obtained for the purpose of examining microcracks in relation to the production of natural gas. The problems of sample preparation for fissile shale have been largely solved. Samples from the NTS have been prepared for the examination of microcracks in relation to possible disposal sites for radioactive waste. |
format |
Report |
author |
Simmons, G. Caruso, L. Padovani, E. |
author_facet |
Simmons, G. Caruso, L. Padovani, E. |
author_sort |
Simmons, G. |
title |
Microcrack technology. Progress report, 1 April 1979-29 February 1980 |
title_short |
Microcrack technology. Progress report, 1 April 1979-29 February 1980 |
title_full |
Microcrack technology. Progress report, 1 April 1979-29 February 1980 |
title_fullStr |
Microcrack technology. Progress report, 1 April 1979-29 February 1980 |
title_full_unstemmed |
Microcrack technology. Progress report, 1 April 1979-29 February 1980 |
title_sort |
microcrack technology. progress report, 1 april 1979-29 february 1980 |
publisher |
Massachusetts Institute of Technology. Department of Earth and Planetary Sciences. |
publishDate |
1980 |
url |
https://doi.org/10.2172/5697427 https://digital.library.unt.edu/ark:/67531/metadc1090417/ |
long_lat |
ENVELOPE(-61.422,-61.422,-62.841,-62.841) |
geographic |
Conway |
geographic_facet |
Conway |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
rep-no: DOE/ER/04972-2 grantno: AC02-78ER04972 doi:10.2172/5697427 osti: 5697427 https://digital.library.unt.edu/ark:/67531/metadc1090417/ ark: ark:/67531/metadc1090417 |
op_doi |
https://doi.org/10.2172/5697427 |
_version_ |
1766134496953892864 |