The article describes the informational and methodological support of the aerospace monitoring of a sea shelf for revealing the temperature and optical anomalies over the deposits of hydrocarbons. The geology-geophysical and hydrophysical factors, as the most important ones, affecting the efficiency of the searching for hydrocarbon deposits are considered. It is established that, between the hydrophysical and hydrodynamic processes in near-surface water layers on the boundary between water and atmosphere, dynamical processes in a fluid, geological structure of the lithosphere, and underwater landscapes, there is an interconnection that should be taken into account, when detecting the hydrocarbon deposit, by using the remote sensing.
In the area of the Krivoy Rog-Kremenchug suture zone, the optical characteristics of landscape elements were studied, both at iron ore deposits and above predicted morphostructures on iron ore deposits. Within the predicted morphostructures with a high magnetic field (iron ore rocks of the Krivoy Rog series), measurements were made of the spectral brightness coefficient (CMF) of vegetation cover. The Landsat-8 satellite image was used to perform spectrometry analysis using factor analysis (factor analysis 2 was most indicative) and elevated values of the optical characteristics of vegetation within the morphostructures above ferruginous rocks were revealed. This made it possible to predict deposits of iron ores within the predicted morphostructures with a high magnetic field intensity.
На конкретному геолого-геофізичному та аерокосмічному матеріалі обґрунтовується припущення про те, що кам'яний пагорб молочанських пісковиків на північ від Мелітополя на правому березі р. Молочна під назвою Кам'яна Могила утворився в кальдері бокового жерла вулкану, розміщеного дещо на південь, унаслідок розмиву долини ріки. Ключові слова: Кам'яна Могила; молочанські пісковики; Оріхово-Павлоградська зона; тектоноконцентр; трансгресія моря; палеовулкан; бокова кальдера палеовулкану.
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