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

Philanthropist

書目名稱Geodynamics of Iceland and the North Atlantic Area影響因子(影響力)




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書目名稱Geodynamics of Iceland and the North Atlantic Area網(wǎng)絡(luò)公開度學(xué)科排名




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書目名稱Geodynamics of Iceland and the North Atlantic Area被引頻次學(xué)科排名




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書目名稱Geodynamics of Iceland and the North Atlantic Area讀者反饋學(xué)科排名

Spongy-Bone

monologue

消耗

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

閑逛

Synapse

Synapse

Preamble

,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

迎合

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

疲勞

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