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Titlebook: Geodynamics of Iceland and the North Atlantic Area; Proceedings of the N L. Kristjansson Conference proceedings 1974 D. Reidel Publishing C

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書(shū)目名稱(chēng)Geodynamics of Iceland and the North Atlantic Area
副標(biāo)題Proceedings of the N
編輯L. Kristjansson
視頻videohttp://file.papertrans.cn/384/383124/383124.mp4
叢書(shū)名稱(chēng)Nato Science Series C:
圖書(shū)封面Titlebook: Geodynamics of Iceland and the North Atlantic Area; Proceedings of the N L. Kristjansson Conference proceedings 1974 D. Reidel Publishing C
描述During the revolution in earth science that has taken place in recent years, studies of the North Atlantic ocean floor and of Iceland have played an increasingly significant role. Icelandic geoscientists have followed, and taken part in, these studies with a keen interest; one of the first tasks of the Geoscience Society of Iceland was to organize an Icelandic symposium on "Iceland and Mid-Ocean Ridges" in 1967. At the suggestion of Dr. G. Pfuason, the Society and various local research institutions formed in 1972 an Organizing Committee for an international meeting on earth science. It was decided that it should be devoted to examining the various expressions of geo~namical forces in the North Atlantic area, in particular at the ocean ridges passing through Iceland. Apart from the scientific content of such a meeting, the organizers also felt it was highly important for scientists from both sides of the Atlantic to meet in Iceland, to become acquainted with recent progress in earth science research there and to coordinate their future research projects in the area. The meeting was held in Reykj avik 1 - 7 July, 1974, and was followed by field trips in Iceland. Generous financial s
出版日期Conference proceedings 1974
關(guān)鍵詞Atlantic Ocean; Topography; chemistry; continental drift; earthquake; evolution; geodynamics; geoscience; li
版次1
doihttps://doi.org/10.1007/978-94-010-2271-2
isbn_softcover978-94-010-2273-6
isbn_ebook978-94-010-2271-2Series ISSN 1389-2185
issn_series 1389-2185
copyrightD. Reidel Publishing Company, Dordrecht 1974
The information of publication is updating

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Deep Drill Investigations of the Oceanic Crust in the North Atlantic,ve enabled us to construct quite detailed models of the structure and evolution of these three tectonic ally and chronologically distinct regions of the North Atlantic ocean floor..Deep Drill 1971 yielded six oriented rock cores from the median valley of the MAR at 45°N. In the resultant model for 4
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,Chemistry of Tholeiitic Basalts from Iceland and their Relation to the Kverkfj?ll Hot Spot,ted” nature of Icelandic basalts has become increasingly apparent [3–6]. This, in conjunction with the high elevation of Iceland relative to the Mid-Atlantic Ridge, and its anomalous volcanic productivity throughout 70 m.y. (as witnessed by the aseismic Wyville-Thompson ridge) has clearly defined Ic
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The Petrologic Nature of the Lower Oceanic Crust and Upper Mantle,e velocities in rocks. Four compositional models for the lower oceanic crust are considered: 1) partially serpentinized peridotite, 2) gabbro, 3) metabasalt and metagabbro and 4) an ophiolite model consisting of metamorphosed sheeted dikes overlying late differentiates and cumulate gabbros. Comparis
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The Structure of Eastern Iceland,he position of the original top of the crust to be deduced. The top lies generally well above the present summit levels, but is highest in the belt of country within which the highest summits occur. There is also a general rise southwards along the length of the belt to a maximum in the Quaternary v
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