Thermochemical Remanent Magnetization and Thermal Remanent Magnetization: Comparison in a Basalt
- 6 November 1970
- journal article
- other
- Published by American Association for the Advancement of Science (AAAS) in Science
- Vol. 170 (3958), 628-630
- https://doi.org/10.1126/science.170.3958.628
Abstract
An improved solution for the gravity field shows ocean rises, as well as trench and island arcs, as mass excesses. Ocean basins, areas of recent glaciation, and the Asian portion of the Alpide belt are mass deficiencies. Most features appear interpretable as varying behavior of the lithosphere in response to asthenospheric flow.Keywords
This publication has 9 references indexed in Scilit:
- Low- and high-temperature oxidation of titanomagnetite in relation to irreversible changes in the magnetic properties of submarine basaltsJournal of Geophysical Research, 1970
- Rotational hysteresis study of oxidized basaltsJournal of Geophysical Research, 1970
- Magnetic properties and oxidation of iron-titanium oxide minerals in Alae and Makaopuhi Lava Lakes, HawaiiJournal of Geophysical Research, 1969
- Magnetization of Ocean BasaltsJournal of geomagnetism and geoelectricity, 1968
- Study of Self-reversal of TRM in Some Submarine BasaltsJournal of geomagnetism and geoelectricity, 1968
- A SPINNER MAGNETOMETER WITH A MAGNETICALLY SHIELDED COILGeophysics, 1967
- Iron-titanium oxides and oxygen fugacities in volcanic rocksJournal of Geophysical Research, 1967
- Thermo-chemical Remanent Magnetization of RocksNature, 1963
- Oxidation of Iron-Titanium Oxides in Igneous RocksThe Journal of Geology, 1962