2022
DOI: 10.1016/j.marpetgeo.2022.105911
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3D stratigraphic mapping and reservoir architecture of the Balakhany Suite, Upper Productive Series, using UAV photogrammetry: Yasamal Valley, Azerbaijan

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Cited by 3 publications
(6 citation statements)
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“…Petrographic, mineralogical and chemical comparisons of all solid ejects from the mud volcanoes at Hamamdagh, Bendovan, Garasu, Khara-Zire and Sangi-Mughan with lithofacies description and the interpretation of several Productive Series outcrops from the South Caspian Basin by Hinds et al [25] suggests that the majority of the mud, mud/claystones and sandstones are sourced from Pleistocene-Pliocene-aged intervals located in ~1 to 4 km depth, corroborating the calculated fluid generation temperatures (~30 ± 10 °C) and depths (~1-4 km depth). Moreover, Upper Productive Series strata found in several outcrops across the Absheron Peninsula (Azerbaijan), such as sandstones and siltto mudstones, have mineralogical compositions that resemble those of the lithogenic fragments described in this study [55]. For example, the fined-grained Yasamal Valley sedimentary rocks mainly comprise quartz (15-40 wt.%), feldspar (10-20 wt.%), calcite (10-25 wt.%) and clay minerals (20-60 wt.%), which mineralogically overlap with the mud and mudstones ejected from the five new mud volcanoes (Table 3).…”
Section: Origin Of Solid Ejectsmentioning
confidence: 54%
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“…Petrographic, mineralogical and chemical comparisons of all solid ejects from the mud volcanoes at Hamamdagh, Bendovan, Garasu, Khara-Zire and Sangi-Mughan with lithofacies description and the interpretation of several Productive Series outcrops from the South Caspian Basin by Hinds et al [25] suggests that the majority of the mud, mud/claystones and sandstones are sourced from Pleistocene-Pliocene-aged intervals located in ~1 to 4 km depth, corroborating the calculated fluid generation temperatures (~30 ± 10 °C) and depths (~1-4 km depth). Moreover, Upper Productive Series strata found in several outcrops across the Absheron Peninsula (Azerbaijan), such as sandstones and siltto mudstones, have mineralogical compositions that resemble those of the lithogenic fragments described in this study [55]. For example, the fined-grained Yasamal Valley sedimentary rocks mainly comprise quartz (15-40 wt.%), feldspar (10-20 wt.%), calcite (10-25 wt.%) and clay minerals (20-60 wt.%), which mineralogically overlap with the mud and mudstones ejected from the five new mud volcanoes (Table 3).…”
Section: Origin Of Solid Ejectsmentioning
confidence: 54%
“…No evidence for sorting (i.e., shift towards the A pole) and K-metasomatism (i.e., shift towards the K pole) is seen. The CIA values are very high compared to basalt (30)(31)(32)(33)(34)(35)(36)(37)(38)(39)(40)(41)(42)(43)(44)(45), granite/granodiorite (45)(46)(47)(48)(49)(50)(51)(52)(53)(54)(55) and feldspar (50), respectively, i.e., they vary in a range from 66 to 74 for all sample types studied among the different localities (Figure 7). This feature suggests that the solid ejects experience post-depositional alterations due to fluid-rock-gas reactions and mud diagenesis.…”
Section: Geochemical Composition Of Solid Ejectsmentioning
confidence: 99%
“…The fifth cluster, called 'environmental monitoring', uses UAVs to detect and quantify methane leaks, as in case studies in the US and Canada [35]. The light blue cluster named 'UAV' reflects its combined use with motion photogrammetry to create a DOM in the Apsheron-Azerbaijan Peninsula [36] and the application of RPAS in the visual inspection of pipelines. The orange cluster called 'drone' includes studies of a hybrid system of monitoring, detection and cleaning of spills, detecting the level of contamination in maritime regions [37].…”
Section: Study Clustersmentioning
confidence: 99%
“…The Mid-Triassic Tredian Formation is well exposed in the western Salt Range and the Surghar Range. This gives scientists a unique chance to study the surface analog for predicting reservoir heterogeneity and facies variations [13,14]. Reservoir heterogeneity is caused by differences in depositional facies, diagenesis, and structural features (such as fractures or faults), and it happens on scales ranging from hundreds of meters to micrometers [14][15][16].…”
Section: Introductionmentioning
confidence: 99%
“…This gives scientists a unique chance to study the surface analog for predicting reservoir heterogeneity and facies variations [13,14]. Reservoir heterogeneity is caused by differences in depositional facies, diagenesis, and structural features (such as fractures or faults), and it happens on scales ranging from hundreds of meters to micrometers [14][15][16]. There are only a few studies conducted on the palynological and paleontological aspects of the Tredian Formation to determine its age and depositional environment [17][18][19][20].…”
Section: Introductionmentioning
confidence: 99%