2018
DOI: 10.1007/s12371-018-0324-x
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Evaluation of Geological Heritage of Geosites for a Potential Geopark in Binh Thuan–Ninh Thuan Coastal Zone, Vietnam

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Cited by 10 publications
(8 citation statements)
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“…The geoheritage sites selection were based on following attributes: phenomenon origin, most visited sites, geographical location (location only within National park/location within Geopark) and significance (scientific, educational or geotouristic). The geodiversity elements, including the high potential for certain types of use, combined with the high degradation risk, demand a higher priority in protection and management policy (Nguyen-Thuy et al, 2018).…”
Section: Discussion Of Resultsmentioning
confidence: 99%
“…The geoheritage sites selection were based on following attributes: phenomenon origin, most visited sites, geographical location (location only within National park/location within Geopark) and significance (scientific, educational or geotouristic). The geodiversity elements, including the high potential for certain types of use, combined with the high degradation risk, demand a higher priority in protection and management policy (Nguyen-Thuy et al, 2018).…”
Section: Discussion Of Resultsmentioning
confidence: 99%
“…The study area has been governed by a part of the Mesozoic continental active margin commonly called Da Lat Zone [36]. This is proven by geological evidence consisting of the calc-alkaline magmatic arcs developed during the late Jurassic-late Cretaceous, such as the Deo Ca complexes of I-type granitoids [36][37][38], the Ankoet complex sourced from a mixture of I and S-type granitoid [39], and the Nha Trang extrusive formation (K nt) [36][37][38]40] (Figure 2a). In the Mesozoic and Cenozoic, the study site was affected by two perpendicular normal fault systems of NW-SE and NE-SW strikes [16] and subparallel fault (Figure 2a).…”
Section: Geology and Hydrogeology Of The Study Sitementioning
confidence: 99%
“…They were formed by complex geodynamic systems changing over time and depended on tide regime and sediment supplies. Generally, coastal sand dunes and bars are part of the Phan Thiet formation (m b Q 1 2−3 pt) (Figure 2a) from the Pleistocene period originating from marine and marine-eolian depositional sources and the weathering alteration of older bedrocks [38,41]. The sediment sequences are characterized by ridges of sand composed mostly of quartz but bearing some heavy minerals such as ilmenite, zircon, anatase, rutile, pyroxene, and monazite [36].…”
Section: Geology and Hydrogeology Of The Study Sitementioning
confidence: 99%
“…LAMP is also cheaper because it only needs a water bath with a constant heat of 60-65 °C instead of a thermal cycler. The efficiency is especially appealing to developing countries with scarce resources and equipment [19,[69][70][71].…”
Section: Crs and Culture As Referencementioning
confidence: 99%