Sedimentation Dynamics of the Lower Part of Sentolo Formation at Niten Stream Traverse, Girimulyo, West Progo

Abstract

Previous geologists showed that Sentolo Formation was interfingering with Jonggrangan Formation and both of them laid unconformably on Old Andesite Formation. The aim of this study is a deeper understanding of the sedimentation dynamics of Sentolo Formation in order to know its stratigraphic relationship to Old Andesite Formation. Petrographic analysis was used to describe the microfacies. Paleontological analysis was used to know the age and sedimentation environment. Stratigraphic measurement of Sentolo Formation in the section of Niten Stream traverse showed that Sentolo Formation was sedimented on the basin environment (SMF3/FZ1; SMF2/FZ1), deep shelf margin (SMF3/FZ3) to foreslope (SMF4/FZ4). The paleontological data indicate that these sedimentary rocks was depositing during Early Miocene until the beginning of Middle Miocene (N6-N9). Sedimentary rock succession is generally dominated by layered limestone with tuff sandstones that develop well in the lower-middle layer. It indicates that the dynamic of basin sedimentation which formed during that period was influenced by volcanic activity that gradually weakened and caused the basin relatively quiet, producing thick limestone.

Study of potential for earthquake acceleration around NYIA, Kulon Progo based on the history of seismicity in Yogyakarta

“…In general, unconformity above the OAF, the Jonggrangan Formation is formed. OAF has a stratigraphic relationship in line with the Sentolo Formation above it [20]. In the Southern Mountains zone, the development of sedimentation begins with the formation of the Gamping-Wungkal Formation during the Eocene.…”

Conservation Design and Scenario for Flood Mitigation on Arui Watershed, Indonesia

“…Thus, groundwater pollution level will mostly be determined by aquifer position, aquifer physical quantity and types along with the types of soil or rocks in the non-saturated zone, and aquifer stone construction (Brickera et al, 2017). Groundwater refers to either rainwater directly absorbed into the soil (Pambudi et al, 2013), or infiltrated runoff, or water stored in organic waste and eventually absorbed by the soil. Canalization is expected to decrease groundwater content and to gradually improve the soil pH.…”