Западная Анатолия тектонически является регионом расширения, и многие системы горст-грабена были разработаны в этом тектоническом режиме. Район Булдан расположен в северной части области Денизли между Денизлинским и Алашехирским грабенами, где наблюдается сейсмическая активность и встречаются горячие источники. Структурное строение разрезов этого района было исследовано с помощью аэромагнитных и гравитационных данных Буге. Для определения тектонических линеаментов были использованы производные метода обнаружения краев (выделения границ); горизонтальный градиент, угол наклона и карта Тета. Карта рельефа подстилающих отложений изученного района была дополнена 3D инверсией гравитационных данных с использованием алгоритма Паркера-Ольденбурга. Окончательная карта гравитационных и магнитных линеаментов исследуемого района представлена как совместная интерпретация результатов процесса обнаружения краев (выделения границ) и карт – рельефа подстилающих отложений, существующей геологической, а также цифровой топографической карты рельефа исследуемого района. Толщина подстилающих пород колеблется в пределах от 0.2 км до 2.2 км, а осадочных пород в северной части бассейна Денизли достигает 2.2 км. Между грабенами Алашехир и Денизли на карте рельефа подстилающих отложений были обнаружены рельефы СЗ-ЮВ простирания, а также линеаменты, такие как сдвиг/трещина, СЗ-ЮВ направления, которые ограничивают рельеф подстилающих отложений. Новые линеаменты в значительной степени совместимы с региональной тенденцией геологического развития района и рельефом подстилающих отложений. Обнаруженные в результате этого исследования новые гравитационные и магнитные линеаменты облегчат понимание тектонического строения, геотермального потенциала, минерализации региона при проведении будущих исследований.

 

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