Abstract
A new multi-anvil type high-presure apparatus has been developed using sintered diamond anvils to generate pressures over 30 GPa and temperatures up to about 2000°C. A maximum sample volume of about 1 mm3 is available in this system. The pressure was confirmed by dissociation of forsterite into Mg-perovskite and periclase. The basic techniques and problems in utilizing sintered diamond in the MA8 type high-pressure apparatus are discussed with an emphasis on the future prospect of incorporating simultaneous X-ray diffraction observation.
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© 1993 Springer Basel AG
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Kondo, T. et al. (1993). The Use of Sintered Diamond Anvils in the MA8 Type High-pressure Apparatus. In: Liebermann, R.C., Sondergeld, C.H. (eds) Experimental Techniques in Mineral and Rock Physics. Pageoph Topical Volumes. Birkhäuser, Basel. https://doi.org/10.1007/978-3-0348-5108-4_20
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DOI: https://doi.org/10.1007/978-3-0348-5108-4_20
Publisher Name: Birkhäuser, Basel
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Online ISBN: 978-3-0348-5108-4
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