Stratigraphic, Mineralogical and Physical Variations at Waikato - North Head, South Auckland: Preliminary Results

- Organization:
- The Australasian Institute of Mining and Metallurgy
- Pages:
- 10
- File Size:
- 1087 KB
- Publication Date:
- Jan 1, 2001
Abstract
Located at the southern end of the Awhitu Peninsula, the Waikato North Head ironsand mine is approximately 50 km southwest of Auckland . The ironsand deposit consists of Quaternary sands, clays and peats, formed by aeolian and marine processes. We sampled on widely- and closely-spaced intervals to test variability within the mining area. X-Ray powder diffraction shows that samples contain feldspars, quartz, pyroxenes, amphiboles, clays and titanomagnetite. Densities range from 1.6 to 2.5 grams/cubic centimetre, with porosities from 30 to 43 percent. The percentage of magnetic minerals values range from 0 to 75 percent, slimes (clay minerals) values of 0 to 26 percent and non-magnetic minerals from 20 to 95 percent. Mineralogical differences in the Mitiwai Formation and Waiuku Blacksand Member cause bimodal populations in the density, magnetic minerals, nonmagnetic minerals and slimes plots. The Mitiwai Formation has higher non-magnetic mineral values and lower density, slimes and magnetic mineral values than the Waiuku Blacksand Member.
Citation
APA:
(2001) Stratigraphic, Mineralogical and Physical Variations at Waikato - North Head, South Auckland: Preliminary ResultsMLA: Stratigraphic, Mineralogical and Physical Variations at Waikato - North Head, South Auckland: Preliminary Results. The Australasian Institute of Mining and Metallurgy, 2001.