Macquarie Island and the Cause of Oceanic Linear Magnetic Anomalies
- 10 October 1969
- journal article
- other
- Published by American Association for the Advancement of Science (AAAS) in Science
- Vol. 166 (3902), 230-233
- https://doi.org/10.1126/science.166.3902.230
Abstract
Macquarie Islands is formed of probably Pliocene oceanic crust. Intruded into pillow lavas is a belt of harzburgite and layered gabbro mnasses cut by dike swarms. Similar belt-like structures may cause the linear magnetic anomalies of the ocean.Keywords
This publication has 16 references indexed in Scilit:
- Pleistocene Climates and Chronology in Deep-Sea SedimentsScience, 1968
- The Mid-Atlantic Ridge near 45° N. II. Basalts from the area of Confederation PeakCanadian Journal of Earth Sciences, 1968
- Palmer Ridge: a Section through the Upper Part of the Ocean Crust?Nature, 1967
- Basalts from the Northern Part of the Mid-Atlantic RidgeJournal of Petrology, 1966
- Chemical Characteristics of Oceanic Basalts and the Upper MantleGSA Bulletin, 1965
- Basalts from the deep ocean floorMineralogical Magazine and Journal of the Mineralogical Society, 1965
- Basalts from the Northern Part of the Rift Zone of the Mid-Atlantic RidgeJournal of Petrology, 1964
- Magnetic Anomalies Over Oceanic RidgesNature, 1963
- Continent and Ocean Basin Evolution by Spreading of the Sea FloorNature, 1961
- Australasian Antarctic Expedition, 1911-1914The Geographical Journal, 1914