Indonesia
Indonesia
Indonesia
Indonesia
VAC 1.6 Науки о Земле и окружающей среде
UDK 550.389 Магнитные съемки. Карты. Данные обсерваторий
UDK 550.380 Техника геомагнитных исследований. Методы наблюдений и измерений. Методика. Оборудование
UDK 550.312 Сила тяжести и изостазия (теория равновесия). Распределение плотности. Распределение силы тяжести
UDK 550.83.04 Наблюдения. Съемка геофизического поля
UDK 550.838 Магнитные методы разведки и съемки
UDK 55 Геология. Геологические и геофизические науки
UDK 550.34 Сейсмология
UDK 550.383 Главное магнитное поле Земли
GRNTI 37.15 Геомагнетизм и высокие слои атмосферы
GRNTI 37.01 Общие вопросы геофизики
GRNTI 37.25 Океанология
GRNTI 37.31 Физика Земли
GRNTI 38.01 Общие вопросы геологии
GRNTI 36.00 ГЕОДЕЗИЯ. КАРТОГРАФИЯ
GRNTI 37.00 ГЕОФИЗИКА
GRNTI 38.00 ГЕОЛОГИЯ
GRNTI 39.00 ГЕОГРАФИЯ
GRNTI 52.00 ГОРНОЕ ДЕЛО
OKSO 05.06.01 Науки о Земле
BBK 263 Геологические науки
BBK 26 Науки о Земле
TBK 6324 Геоэлектричество. Геомагнетизм
TBK 63 Науки о Земле. Экология
BISAC SCI SCIENCE
Bawean Island is a result of volcanic activity in the back-arc volcanism zone located on the north side of Java Island. Bawean Island was formed due to the geological structure being controlled by the Paleogene-Neogene tectonic line in the Meratus Pattern. The mantle tearing resulted in the formation of the Bawean Arc. The Kepuhlegundi Hot Spring is a component of the volcanism product on Bawean Island. To analyze the formation of hot springs in more detail, we conducted magnetic method measurements and integrated the data with gravity satellite and Fault Fracture Density (FFD) methods. The three methods were used to determine the continuity of the mapped geological structures surrounding the hot springs. The FFD method can be used to map the weak zone of the hot spring, which is caused by the lineament surrounding it. The magnetic and gravity methods reveal anomalous contrasts that extend towards the hot springs in the direction of the structure. The magnetic and gravity methods reveal anomalous contrasts that extend towards the hot springs in the direction of the structure. Based on regional anomaly analysis, spectrum analysis indicates that the structure is located at a shallow depth of 15 to 80 meters. The drawing in each method shows a dominant orientation in the Northeast-Southwest direction, which corresponds to the orientation of the Meratus Structure Pattern. Kepuhlegundi Hot Spring is formed due to the control of geological structures, allowing hot fluids to flow through fractures as an aquifer.
bawean, hot spring, geological structure, fault fracture density, magnetic, gravity, aquifer
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