
); Poisson's ratio (µ); Young's modulus(E); Shear modulus(G), Debye temperature(
) etc.The materials were selected from natural outcrops of Magellan (one sample), New Canton (2 samples), Clarion (5 samples) transform faults Central Pacific by dragging of 28th Mendeleev research vessel trip (1982). Petrographic characterization was made on the base of optical determinations. The results show that their physical properties vary in very large limits (see table).| Pef | | Vp | Vs | µ | E | G | ![]() | ||
| No | Rock type | % | t/m3 | m/s | m/s | - | 10GPa | 10GPa | K |
| 1 | Variolite hyaline basalt | 22.01 | 2.21 | 3622 | 2233 | 0.19 | 2.58 | 1.08 | 289 |
| 2 | Volcanic breccia | 10.17 | 2.54 | 4241 | 2667 | 0.17 | 4.15 | 1.77 | 361 |
| 4 | Dolerite | 1.19 | 2.95 | 5727 | 3369 | 0.24 | 8.10 | 3.28 | 471 |
| 5 | Aphyric amygdaloidal basalt | 20.37 | 2.22 | 3513 | 2426 | 0.04 | 2.68 | 1.28 | 310 |
| 6 | Gabbro | 4.08 | 2.79 | 4785 | 2985 | 0.18 | 5.77 | 2.44 | 413 |
| 7 | Gabbro | 5.71 | 2.79 | 5674 | 3218 | 0.26 | 7.15 | 2.83 | 450 |
| 8 | Basalt | 17.12 | 2.38 | 4004 | 2365 | 0.23 | 3.22 | 1.31 | 315 |
| 9 | Fine grained quartz rock | 35.05 | 1.71 | 3718 | 2085 | 0.27 | 1.85 | 0.73 | 250 |
| 10 | Basalt | 19.14 | 2.27 | 3726 | 2318 | 0.18 | 2.84 | 1.20 | 302 |
This is a consequence of the very different rocks forming conditions. The betterplanning and special specimens collecting will significantly improve the petrophysicalmarine investigations, which with their productivity, simplicity, low costs and highlyinformativity will help very much in better describing and understanding of ocean floorforming processes.
1. Starostin, V. I. 1979. Structure-petrophysical analysis of endogenous ore fields. Nedra,Moscow, 257 p. (in Russian)
Abstract Source:
Book of Abstracts, 7th European Conference on Non-Destructive Testing, 26-29 May 1998, ISBN: 87-986898-0-00
Full-Text Source:
Proceedings of the 7th European Conference on Non-Destructive Testing, 26-29 May 1998, ISBN:
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