Carol A Finn, Ph.D. (Former Employee)
Science and Products
Filter Total Items: 131
Improved geomagnetic referencing in the Arctic environment Improved geomagnetic referencing in the Arctic environment
Geomagnetic referencing uses the Earth’s magnetic field to determine accurate wellbore positioning essential for success in today's complex drilling programs, either as an alternative or a complement to north-seeking gyroscopic referencing. However, fluctuations in the geomagnetic field, especially at high latitudes, make the application of geomagnetic referencing in those areas more...
Authors
B. Poedjono, N. Beck, A. C. Buchanan, L. Borri, S. Maus, Carol Finn, E. William Worthington, Tim White
Regional tectonic setting for the Trinidad earthquake swarms (2000-2012) from gravity and magnetic data Regional tectonic setting for the Trinidad earthquake swarms (2000-2012) from gravity and magnetic data
Earthquakes in the Raton basin near Trinidad, Colorado, (Figure 1) are located (Rubenstein et. al., 2014) near a major gravity and magnetic boundary. These earthquakes also occur in an area of hydrocarbon production that includes several high-capacity produced water injection wells. This presentation gives a very basic outline of the relation between the earthquakes, the potential field...
Authors
Carol A. Finn, Mason A. Kass, Bruce D. Smith
The Boulder magnetic observatory The Boulder magnetic observatory
The Boulder magnetic observatory has, since 1963, been operated by the Geomagnetism Program of the U.S. Geological Survey in accordance with Bureau and national priorities. Data from the observatory are used for a wide variety of scientific purposes, both pure and applied. The observatory also supports developmental projects within the Geomagnetism Program and collaborative projects with...
Authors
Jeffrey J. Love, Carol A. Finn, Kolby L. Pedrie, Cletus C. Blum
Mapping the 3-D extent of the Northern Lobe of the Bushveld layered mafic intrusion from geophysical data Mapping the 3-D extent of the Northern Lobe of the Bushveld layered mafic intrusion from geophysical data
Geophysical models image the 3D geometry of the mafic portion of the Bushveld Complex north of the Thabazimbi-Murchison Lineament (TML), critical for understanding the origin of the world's largest layered mafic intrusion and platinum group element deposits. The combination of the gravity and magnetic data with recent seismic, MT, borehole and rock property measurements powerfully...
Authors
Carol A. Finn, Paul A. Bedrosian, Janine Cole, Tshepo David Khoza, Susan J. Webb
Crystalline basement map of Mauritania derived from filtered aeromagnetic data (deliverable 54_1), Aeromagnetic and geological structure map of Mauritania (phase V, deliverable 54_2), Maximum depth to basement map of Mauritania derived from Euler analysis Crystalline basement map of Mauritania derived from filtered aeromagnetic data (deliverable 54_1), Aeromagnetic and geological structure map of Mauritania (phase V, deliverable 54_2), Maximum depth to basement map of Mauritania derived from Euler analysis
In 1996, at the request of the Government of the Islamic Republic of Mauritania, a team of U.S. Geological Survey (USGS) scientists produced a strategic plan for the acquisition, improvement and modernization of multidisciplinary sets of data to support the growth of the Mauritanian minerals sector and to highlight the geological and mineral exploration potential of the country. In 1999...
Authors
Carol A. Finn, John D. Horton
Synthesis of geophysical data (phase V, deliverable 55) Synthesis of geophysical data (phase V, deliverable 55)
Aeromagnetic and radiometric data were used to map shallow Precambrian basement lithology and structure and determine the depth to magnetic basement, which in most cases, corresponds to the depth to crystalline basement of interest for mineral exploration. These depths, along with those determined from gravity data, help identify basins with hydrologic potential. In addition, the...
Authors
Carol A. Finn, Eric D. Anderson
Science and Products
Filter Total Items: 131
Improved geomagnetic referencing in the Arctic environment Improved geomagnetic referencing in the Arctic environment
Geomagnetic referencing uses the Earth’s magnetic field to determine accurate wellbore positioning essential for success in today's complex drilling programs, either as an alternative or a complement to north-seeking gyroscopic referencing. However, fluctuations in the geomagnetic field, especially at high latitudes, make the application of geomagnetic referencing in those areas more...
Authors
B. Poedjono, N. Beck, A. C. Buchanan, L. Borri, S. Maus, Carol Finn, E. William Worthington, Tim White
Regional tectonic setting for the Trinidad earthquake swarms (2000-2012) from gravity and magnetic data Regional tectonic setting for the Trinidad earthquake swarms (2000-2012) from gravity and magnetic data
Earthquakes in the Raton basin near Trinidad, Colorado, (Figure 1) are located (Rubenstein et. al., 2014) near a major gravity and magnetic boundary. These earthquakes also occur in an area of hydrocarbon production that includes several high-capacity produced water injection wells. This presentation gives a very basic outline of the relation between the earthquakes, the potential field...
Authors
Carol A. Finn, Mason A. Kass, Bruce D. Smith
The Boulder magnetic observatory The Boulder magnetic observatory
The Boulder magnetic observatory has, since 1963, been operated by the Geomagnetism Program of the U.S. Geological Survey in accordance with Bureau and national priorities. Data from the observatory are used for a wide variety of scientific purposes, both pure and applied. The observatory also supports developmental projects within the Geomagnetism Program and collaborative projects with...
Authors
Jeffrey J. Love, Carol A. Finn, Kolby L. Pedrie, Cletus C. Blum
Mapping the 3-D extent of the Northern Lobe of the Bushveld layered mafic intrusion from geophysical data Mapping the 3-D extent of the Northern Lobe of the Bushveld layered mafic intrusion from geophysical data
Geophysical models image the 3D geometry of the mafic portion of the Bushveld Complex north of the Thabazimbi-Murchison Lineament (TML), critical for understanding the origin of the world's largest layered mafic intrusion and platinum group element deposits. The combination of the gravity and magnetic data with recent seismic, MT, borehole and rock property measurements powerfully...
Authors
Carol A. Finn, Paul A. Bedrosian, Janine Cole, Tshepo David Khoza, Susan J. Webb
Crystalline basement map of Mauritania derived from filtered aeromagnetic data (deliverable 54_1), Aeromagnetic and geological structure map of Mauritania (phase V, deliverable 54_2), Maximum depth to basement map of Mauritania derived from Euler analysis Crystalline basement map of Mauritania derived from filtered aeromagnetic data (deliverable 54_1), Aeromagnetic and geological structure map of Mauritania (phase V, deliverable 54_2), Maximum depth to basement map of Mauritania derived from Euler analysis
In 1996, at the request of the Government of the Islamic Republic of Mauritania, a team of U.S. Geological Survey (USGS) scientists produced a strategic plan for the acquisition, improvement and modernization of multidisciplinary sets of data to support the growth of the Mauritanian minerals sector and to highlight the geological and mineral exploration potential of the country. In 1999...
Authors
Carol A. Finn, John D. Horton
Synthesis of geophysical data (phase V, deliverable 55) Synthesis of geophysical data (phase V, deliverable 55)
Aeromagnetic and radiometric data were used to map shallow Precambrian basement lithology and structure and determine the depth to magnetic basement, which in most cases, corresponds to the depth to crystalline basement of interest for mineral exploration. These depths, along with those determined from gravity data, help identify basins with hydrologic potential. In addition, the...
Authors
Carol A. Finn, Eric D. Anderson
*Disclaimer: Listing outside positions with professional scientific organizations on this Staff Profile are for informational purposes only and do not constitute an endorsement of those professional scientific organizations or their activities by the USGS, Department of the Interior, or U.S. Government