Diagenesis of magnetic mineral assemblages in multiply redeposited siliciclastic marine sediments, Wanganui basin, New Zealand

Author:

Wilson Gary S.,Roberts Andrew P.

Publisher

Geological Society of London

Subject

Geology,Ocean Engineering,Water Science and Technology

Reference58 articles.

1. The sequence architecture of mid-Pleistocene (c. 1.1–0.4 Ma) cyclothems from New Zealand: facies development during a period of orbital control on sea level cyclicity;Abbott,1994

2. Mössbauer effect observations of the ‘x-phase’ in the ilmenite-hematite series;Allen;Journal of Geomagnetism and Geoelectricity,1974

3. Structure and evolution of the South Wanganui Basin, New Zealand;Anderton;New Zealand Journal of Geology and Geophysics,1981

4. Sedimentary pyrite formation

5. Sedimentary pyrite formation: An update

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