1980 Articles
Magnetic components contributing to the NRM of Middle Siwalik red beds
The components of the NRM in Middle Siwalik red beds are carried by two phases of hematite, a red pigment phase and a specular hematite phase. We present evidence in the form of a conglomerate test that the specularite phase carries a remanence acquired during or shortly after deposition. The red pigment, however, post-dates deposition, in many cases by at least one reversal boundary. This secondary component has a higher coercivity but a lower blocking temperature in these rocks and can therefore be selectively removed by thermal demagnetization to reveal a primary magnetization useful for magnetostratigraphic studies.
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Also Published In
- Title
- Earth and Planetary Science Letters
- DOI
- https://doi.org/10.1016/0012-821X(80)90044-8
More About This Work
- Academic Units
- Lamont-Doherty Earth Observatory
- Biology and Paleo Environment
- Published Here
- December 5, 2011