Геология и минеральные ресурсы Мирового Океана. В. Н. Судариков

Геология и минеральные ресурсы Мирового Океана

гребней, гряд, сложенных застывшими при трещинных излияниях лавами, зияющими тектоническими трещинами и крупными вулканами (более 20 действующих).

По современным данным разрез земной коры в районе Исландии сходен с разрезом континентальной коры, но отличается очень мощным «базальтовым» слоем, присутствием слоя повышенной плотности, глубоким залеганием поверхности Мохоровичича (до 50 км) и сильно редуцированным «гранитным» слоем.

Конец ознакомительного фрагмента.

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