Plio-Pleistocene paleoclimate in the Southwest Pacific as reflected in clay mineralogy and particle size at ODP Site 1119, SE New Zealand

Author:

Land Marissa,Wust Raphael A.J.,Robert Christian,Carter Robert M.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology,Oceanography

Reference71 articles.

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2. Distinction between kaolinite and chlorite in recent sediments by X-ray diffraction;Biscaye;American Mineralogist,1964

3. The petrology and alteration of Tertiary Basalts of the Coalgate area, northwest Canterbury;Carlson;Journal of Royal Society of New Zealand,1975

4. The role of intermediate-depth currents in continental shelf-slope accretion: Canterbury Drifts, SW Pacific Ocean;Carter;Geological Society of London,2007

5. Post-breakup stratigraphy of the Kaikoura Synthem (Cretaceous–Cenozoic), continental margin, southeastern New Zealand;Carter;New Zealand Journal of Geology and Geophysics,1988

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