Геотермическое поле зоны перехода между Анатолийской плитой и Восточно-Европейской платформой
Аннотация
В восточной части Средиземного моря выделяют обширную провинцию низкого теплового потока, простирающуюся во всем бассейне моря восточнее Крита (Левантинское море), включая Кипр и северный Египет. Геология территории восточной Анатолии сложна из-за недавней тектонической и вулканической актив ности. Этот регион включает главные тектонические блоки Понтийских гор, Анатолийско-Тавридский пояс и сутурную зону Битлиса, Северо- и Восточно-Анатолийский разломы. Во многих частях Анатолии встречаются офио литы и молодые вулканические породы. Черное море окружено Альпийско-Гималайским складчатым поясом (Крым, Большой Кавказ, Понтийские горы, Родопо-Странджский массив, восточное Среднегорье, Северная Доб руджа) и древними тектоническими блоками различного происхождения и возраста, такими как Восточно-Европейский кратон, Мизийская платформа, Стамбульская зона и Аджаро-Триалетская складчатая система. В Черном море преобладает низкий теп ловой поток. Наименьшие значения (менее 30 мВт/м2 ) зарегистрированы в центральных частях западного и восточного бассейнов Черного моря с максимальной мощностью осадочных отложений. Геотермические исследования на территории Украины ведутся в течение 45 лет. Многие особенности теплового поля остаются неизученными. Это относится, в частности, к Украинскому щиту и южной части региона Карпат. В целом территория альпийской складчатости в пределах Турции, Мраморного и Эгейского морей, Кавказа характеризуется высоким тепловым потоком. Аномалия его наибольших значений (более 100 –150 мВт/м2 ) отмечается на западе Турции, где преобладают тектонические условия растяжения и ведется использование подземного пара для выработки электроэнергии. Построены карта и три профиля теплового потока, пересекающих изучаемый регион.
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