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Titlebook: Origins of Igneous Layering; Ian Parsons Book 1987 Springer Science+Business Media Dordrecht 1987 chemistry.formation.igneous rock.mineral

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發(fā)表于 2025-3-21 16:47:16 | 只看該作者 |倒序瀏覽 |閱讀模式
書目名稱Origins of Igneous Layering
編輯Ian Parsons
視頻videohttp://file.papertrans.cn/705/704643/704643.mp4
叢書名稱Nato Science Series C:
圖書封面Titlebook: Origins of Igneous Layering;  Ian Parsons Book 1987 Springer Science+Business Media Dordrecht 1987 chemistry.formation.igneous rock.mineral
描述Acknowledgements xix pioneering workers on igneous layering in Greenland xx Wbrkshop participants xxii Henning Sfl!rensen, University of Copenhagen, Dermark. Latte Melchior Larsen, Geological SUrvey of Greenland, Copenhagen, Dermark. Abstract 1 1 ? Introduction 1 1. 1 The agpaitic rocks of the Ilimaussaq intrusion 3 2. Igneous layering in the Ilimaussaq intrusion 4 3. Mineralogy of the layered kakortokite series 15 4. Chemistry of the layered kakortokite series 19 5. Origin of the kakortokite layering 20 5. 1 Discussion 22 6. Conclusion 25 References 26 2. I. AYERn?;r CCMPlCTIOO NID PCBJ. "--MN}tATIC ~ IN ‘!HE KLOKKEN INTRUSIOO 29 Ian Parsons and SUsanne M. Becker, University of Aberdeen, U. K. Abstract 29 1. Introduction 30 2. Age of the intrusion 31 3. General structure and mineral variation 31 vi TABLE OF CONTENTS 3. 1 Nomenclature of rock types 31 3. 2 Bulk chemical and modal variation 36 4. The contacts and wall-rocks 37 4. 1 Guter contact 37 4. 2 The gabbro sheath 37 4. 3 The unlaminated syenite sheath 39 4. 4 The gabbro-syenite transition 41 5. The layered series 43 5. 1 General relationships 43 5. 2 Granular syenites 43 5. 2. 1 Structure and cryptic variation 43 5. 2. 2 Ori
出版日期Book 1987
關鍵詞chemistry; formation; igneous rock; mineral; mineralogy; pattern formation
版次1
doihttps://doi.org/10.1007/978-94-017-2509-5
isbn_softcover978-90-481-8435-4
isbn_ebook978-94-017-2509-5Series ISSN 1389-2185
issn_series 1389-2185
copyrightSpringer Science+Business Media Dordrecht 1987
The information of publication is updating

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1389-2185 ro-syenite transition 41 5. The layered series 43 5. 1 General relationships 43 5. 2 Granular syenites 43 5. 2. 1 Structure and cryptic variation 43 5. 2. 2 Ori978-90-481-8435-4978-94-017-2509-5Series ISSN 1389-2185
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A. J. Naldrett,G. Cameron,G. von Gruenewaldt,M. R. Sharpe
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Layering in the Ilimaussaq Alkaline Intrusion, South Greenland,ering and macrorhythmic layering. The mineralogy of the kakortokite series is described, and theories of formation of the layering reviewed. Crystallisation probably took place in a stagnant bottom layer, and the layering is considered to be caused by different nucleation and growth maxima, in relat
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The Southern Part of the Fongen-Hyllingen Layered Mafic Complex, Norway: Emplacement and Crystallize wall, varying over 7km from Fo.:An. to Fo.:An.. The apparent angle between cryptic and modal layering is usually less than 20°. The start of the major regression, reflecting the influx of fresh magma at the floor of the chamber, is concordant with modal layering which implies that modal layering r
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