Results 251 to 260 of about 2,609 (307)
Mechanisms of clay mineral-induced targeted deposition and synergistic CO2 sequestration potential in the CCUS-EOR process. [PDF]
Zhang M +7 more
europepmc +1 more source
Geophysical insights from the first geomagnetic field absolute intensity curve for central Asia (2200BCE-2000CE), and implications for archaeomagnetic dating. [PDF]
Bonilla-Alba R +8 more
europepmc +1 more source
Magnetic dipole imaging of magnetite nanoparticles in brain tissue. [PDF]
Kaub L +8 more
europepmc +1 more source
Revealing porphyry mineralization Cu-Au signatures via analyzing aeromagnetic and remote sensing data of Dara-Monqul, area Egypt. [PDF]
Abdellatif M +5 more
europepmc +1 more source
Some of the next articles are maybe not open access.
Related searches:
Related searches:
Reviews of Geophysics, 1983
I have the responsibility of reviewing the advances made in rock magnetism (and paleomagnetic data analysis) over the last four years. My charge includes the specific invitation to comment on the use of rock magnetism in the service of paleomagnetism. This is, of course, a distinction that is often difficult to draw.
Peter N Shive
exaly +2 more sources
I have the responsibility of reviewing the advances made in rock magnetism (and paleomagnetic data analysis) over the last four years. My charge includes the specific invitation to comment on the use of rock magnetism in the service of paleomagnetism. This is, of course, a distinction that is often difficult to draw.
Peter N Shive
exaly +2 more sources
Rock Magnetism, first published in 1997, is a comprehensive treatment of fine particle magnetism and the magnetic properties of rocks. Starting from atomic magnetism and magnetostatic principles, the authors explain why domains and micromagnetic structures form in ferromagnetic crystals and how these lead to magnetic memory in the form of thermal ...
David J. Dunlop, Özden Özdemir
openaire +2 more sources
Introduction to the special section on Fundamental and Frontier Research in Rock Magnetism [PDF]
Many of the papers in this special section were first presented in the session “Rock Magnetism: Fundamentals and Frontiers” at the 2005 Fall AGU meeting.
Mike Jackson, Wyn Williams
exaly +2 more sources
International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts, 1995
Rock magnetism is the study of induced and remanent magnetization of ferrimagnetic mineral grains in rocks, sediments, soils, and organisms. Its applications include environmental magnetism, magnetic anisotropy, sources of continental and oceanic magnetic anomalies, records of geomagnetic field variations and polarity reversals, and the paleomagnetic ...
openaire +2 more sources
Rock magnetism is the study of induced and remanent magnetization of ferrimagnetic mineral grains in rocks, sediments, soils, and organisms. Its applications include environmental magnetism, magnetic anisotropy, sources of continental and oceanic magnetic anomalies, records of geomagnetic field variations and polarity reversals, and the paleomagnetic ...
openaire +2 more sources
The Moon, 1972
The relationship between the magnetization and temperature in a high constant magnetic field for a temperature range between 5 K and 1100 K was examined for Apollo 11, 12 and 14 lunar materials. The average value of Curie point temperature is (768.2 ± 3.5)°C for the lunar igneous rocks and (762.5 ± 3.4)°C for the lunar fines and breccias.
T. Nagata, R. M. Fisher, F. C. Schwerer
openaire +1 more source
The relationship between the magnetization and temperature in a high constant magnetic field for a temperature range between 5 K and 1100 K was examined for Apollo 11, 12 and 14 lunar materials. The average value of Curie point temperature is (768.2 ± 3.5)°C for the lunar igneous rocks and (762.5 ± 3.4)°C for the lunar fines and breccias.
T. Nagata, R. M. Fisher, F. C. Schwerer
openaire +1 more source
1956
The main topic of this chapter is the discussion of the natural remanent magnetization of rocks with the object of inferring the direction of the geomagnetic field in the geological past. The reader who is interested in other aspects of rock magnetism is referred to the additional references at the end.
openaire +1 more source
The main topic of this chapter is the discussion of the natural remanent magnetization of rocks with the object of inferring the direction of the geomagnetic field in the geological past. The reader who is interested in other aspects of rock magnetism is referred to the additional references at the end.
openaire +1 more source

