On microlocation of submarine karstic sulpur springs near Izola: a small correction makes again a crucial difference
نویسندگان
چکیده
In the Slovenian part of Gulf Trieste/Trst, submarine springs occur as funnel-shaped depressions in Holocene sandy-silt marine sediment that forms seafloor. These exhibit both elevated temperatures (up to 29.6 °C) and sulphur content. Based on their location, they are divided into three groups: Izola group (three springs), Bele skale (two Ronek (seven springs). Previous investigations linked these anticline, characterized by its limestone core flysch limbs, but no detailed explanation was provided. We propose that: A) groundwater from (karstic aquifer) at stratigraphic boundary with B) nearshore area, where sedimentary cover Quaternary deposits is thin enough be penetrated spring waters washed out. According existing data, anticline axis NW-SE directed, lies approximately seaward extension axis. Therefore, this interpretation fits perfectly for group, while groups off-axis extensions require reinterpretation. order resolve micro-locations groups, we conducted a sedimentological logging geological mapping. The revealed outcrops only town Izola, two prominent calciturbidite megabeds enable very mapping, C) oriented WNW-ESE direction, moderate anti-clockwise rotation explains micro locations all springs. located southern side, northern side anticline.
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ژورنال
عنوان ژورنال: Acta Carsologica
سال: 2023
ISSN: ['1580-2612', '0583-6050']
DOI: https://doi.org/10.3986/ac.v52i1.11091