| 000 | 01996nam a2200373 i 4500 | ||
|---|---|---|---|
| 008 | 860309s1983 enka b 100 0 eng | ||
| 010 | _a83192045 | ||
| 020 | _a090681233X | ||
| 020 |
_a0906812348 _q(paperback) |
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| 040 |
_aBAUN _beng _cBAUN _erda |
||
| 049 | _aBAUN_MERKEZ | ||
| 050 | 0 | 4 |
_aQE462.B3 _bC66 1983 |
| 245 | 0 | 0 |
_aContinental basalts and mantle xenoliths / _cC.J. Hawkesworth and M.J. Norry, editors |
| 264 | 1 |
_aNantwich, Cheshire : _bShiva Pub. , _c[1983] |
|
| 264 | 1 |
_aCambridge, MA, USA : _bAvailable in North America from Birkhauser Boston, _c[1983] |
|
| 264 | 4 | _c©1983 | |
| 300 |
_aviii, 272 pages : _billustrations ; _c24 cm |
||
| 336 |
_atext _btxt _2rdacontent |
||
| 337 |
_aunmediated _bn _2rdamedia |
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| 338 |
_avolume _bnc _2rdacarrier |
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| 380 | _aBibliography | ||
| 490 | 0 | _aShiva geology series | |
| 504 | _aBibliography: pages 251-272 | ||
| 505 | 0 | 0 |
_tCompositional differences between oceanic and continental basic lavas and their significance _r/ M.J. Norry and J.G. Fitton _t-- Stable isotope evidence on the nature of crust-mantle interactions _r/ C.M. Graham and R.S. Harmon _t-- Mantle peridotites and processes _r/ B. Harte _t-- Mantle ultramafic xenoliths in alkaline magmas _r/ M. Menzies _t-- Evolution of the continental lithosphere _r/ C.J. Hawkesworth ... [and others] _t-- The Karoo province of southern Africa _r/ K.G. Cox _t-- Continental flood basalts--arachnids rule OK? _r/ R.N. Thompson ... [and others] _t-- Isotope geochemistry and contamination mechanics of Tertiary lavas for Skye, northwest Scotland _r/ M.F. Thirlwall and N.W. Jones _t-- Chemistry of the sub-continental lithosphere in magma genesis at active continental margins _r/ J.A. Pearce |
| 650 | 0 |
_aBasalt _xCongresses |
|
| 650 | 0 |
_aContinents _xCongresses |
|
| 650 | 0 |
_aIgneous rocks _xInclusions _xCongresses |
|
| 651 | 0 |
_aEarth (Planet) _xMantle _xCongresses |
|
| 700 | 1 | _aHawkesworth, C. J | |
| 700 | 1 | _aNorry, M. J | |
| 900 | _a25230 | ||
| 900 | _bbağış | ||
| 942 |
_2lcc _cKT |
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| 999 |
_c22670 _d22670 |
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