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| LEADER |
01934cam a22004697a 4500 |
| 001 |
BIBLO-7578 |
| 003 |
AR-BaUEN |
| 005 |
20201111150127.0 |
| 008 |
201111s1967 xxu||||f |||| 00| 0|eng|d |
| 040 |
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|a AR-BaUEN
|b spa
|c AR-BaUEN
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| 044 |
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|a xxu
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| 080 |
|
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|a 552.3
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| 100 |
1 |
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|a Wager, L. R.
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| 245 |
1 |
0 |
|a Layered igneous rocks
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| 260 |
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|a San Francisco :
|b Freeman,
|c 1967
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| 300 |
|
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|a 1 v.
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| 505 |
0 |
0 |
|t PREFACE
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| 505 |
0 |
0 |
|g I
|t CRYSTAL SETTLING AND THE DIVERSITY OF IGNEOS ROCKS
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| 505 |
0 |
0 |
|g II
|t GENERAL FEATURES OF THE SKAERGAARD INTRUSION
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| 505 |
0 |
0 |
|g III
|t THE MINERALS OF THE SKAERGAARD INTRUSION
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| 505 |
0 |
0 |
|g IV
|t THE SKAERGAARD LAYERED SERIES
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| 505 |
0 |
0 |
|g V
|t THE SKAERGAARD MARGINAL AND UPPER BORDER GROUPS, AND THE GRANOPHYRIC DIFFERENTIATES
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| 505 |
0 |
0 |
|g VI
|t THE BASISTOPPEN SHEET
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| 505 |
0 |
0 |
|g VII
|t THE CHEMISTRY OF THE SKAERGAARD INTRUSION
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| 505 |
0 |
0 |
|g VIII
|t THE MECHANISM OF THE SKAERGAARD DIFFERENTIATION
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| 505 |
0 |
0 |
|g IX
|t THE SKAERGAARD FRACTIONATION TREND AND POSSIBLE EXPLANATIONS
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| 505 |
0 |
0 |
|g X
|t THE RHUM ULTRABASIC COMPLEX, SCOTLAND: FORM OF INTRUSION, UNITS OF LAYERING, AND MINERALS
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| 505 |
0 |
0 |
|g XI
|t RHUM TEXTURES, STRUCTURES, AND LAYERED SEQUENCE
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| 505 |
0 |
0 |
|g XII
|t RHUM CHEMISTRY AND GENESIS
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| 505 |
0 |
0 |
|g XIII
|t THE STILLWATER INTRUSION, MONTANA, U.S.A.
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| 505 |
0 |
0 |
|g XIV
|t THE BUSHVELD INTRUSION, SOUTH AFRICA
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| 505 |
0 |
0 |
|g XV
|t SOME OTHER TYPES OF BASIC LAYERED INTRUSIONS
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| 505 |
0 |
0 |
|g XVI
|t LAYERING IN GRANITES, QUARTZ SYENITES, AND FELSPATHOIDAL SYENITES
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| 505 |
0 |
0 |
|g XVII
|t ADDITIONAL LIST OF LAYERED OR FRACTIONATED INTRUSIONS
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| 505 |
0 |
0 |
|g XVIII
|t DIFFERENTIATED SILLS
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| 505 |
0 |
0 |
|g XIX
|t SOME GENERALIZATIONS ON LAYERED INTRUSIONS
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| 505 |
0 |
0 |
|t REFERENCES
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| 505 |
0 |
0 |
|t SUBJECT INDEX
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| 505 |
0 |
0 |
|t AUTHOR INDEX
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| 700 |
1 |
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|a Brown, G. M.
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| 962 |
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|a info:eu-repo/semantics/book
|a info:ar-repo/semantics/libro
|b info:eu-repo/semantics/publishedVersion
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| 999 |
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|c 7575
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