Наиболее сложными регионами Земли являются области перехода от океана к континенту, а также зоны спрединга и сочленения литосферных плит. Восточное Средиземноморье, являющееся ярким примером вышеуказанных областей, расположено на стыке крупнейших литосферных сегментов Земли: Евразии и Гондваны. Количественный анализ магнитных аномалий выполнен с использованием передовых методик, позволяющих применять интерпретационные процедуры в условиях (1) наклонной намагниченности, (2) пересеченного рельефа местности и (3) наложения аномалий разного ранга. Представлены примеры детального анализа магнитных аномалий для нескольких геологически сложных районов на севере Израиля: Галилейского моря, Кармеля и Малкишона. Методика палеомагнитного картирования таких переходных зон основана на комплексировании методов картирования как континентальных, так и океанических платформ: палеомагнитных реконструкций, результатов радиометрического датирования магнитоактивных пород, изучения спутниковых данных, тектоно-структурных реконструкций, биогеографического анализа и использования результатов различных геофизических исследований. Геодинамическое палеомагнитное картирование позволяет выявить не только многоуровневые структурные неоднородности среды, но и отобразить сложные элементы разновозрастной геодинамики, присущие зонам сочленения (перехода). В северном Израиле для комплексного палеомагнитного картирования были выбраны хорошо изученные палеомагнитными и радиометрическими методами (а также структурно-тектонически) районы: (1) Галилейское море с прилегающими зонами (ранее построенные схемы этих районов были откорректированы и дополнены), (2) район Кармель, и (3) район Атлит (внутренняя часть района Кармель). Построенный палеомагнитный профиль для района Кармель по кровле аккумулятивной поверхности нижнемеловых траппов наглядно показывает сложную историю палеогеодинамического развития региона. Сделан вывод об эффективности сочетания процедур количественной интерпретации магнитных аномалий с палеомагнитным картированием сложных сред. Палинспастическая реконструкция, разработанная для периода 3.6-2.0 млн. лет назад, выявила важные тектоно-магматические особенности этого геологического периода.

Ключевые слова: палеомагнитное картирование, палеомагнитное профилирование, анализ магнитных данных, тектоно-структурная интерпретация, комплексный анализ, палинспастическая реконструкция

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