Growth, destruction and volcanic facies architecture of three volcanic centres in the Miocene Uşak–Güre basin, western Turkey: Subaqueous–subaerial volcanism in a lacustrine setting

Karaoğlu, Özgür; Helvacı, Cahit

doi:10.1016/j.jvolgeores.2012.06.028

Cited by 16 publications

(3 citation statements)

References 65 publications

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“…The onset of sedimentation in the Sinanpaşa Basin, with alluvial lacustrine deposits and a first pulse of volcanic activity, was similar as in the other adjacent grabens, such as the Bigadiç-Balıkesir Basin (Helvacı, 1995), Uşak-Güre Basin (Karaoğlu and Helvacı, 2012), Emet-Kütahya Basin (Helvacı, 1977;Baş, 1986;Helvacı et al, 2017), Kırka-Eskişehir Basin (Helvacı and Orti, 2004), Afyon Basin (Aydar, 1998;Akal et al, 2013;Prelevic et al, 2015), and Şuhut-Sandıklı Basin (Koçyiğit and Deveci, 2007b;Gündoğan et al, 2012). Similar to neighboring grabens, the Sinanpaşa Graben basin has been filled by fluvial alluvial fan deposits (first sedimentary products) since the Early Miocene.…”

Section: Sedimentary Paleoenvironmentmentioning

confidence: 54%

“…volcanic rocks in West Anatolian basins (e.g., the Denizli, Uşak, Bigadiç, and Sinanpaşa basins in the Afyon Zone) are interbedded with widespread Miocene fluvial-lacustrine deposits reaching more than 1000 m in thickness (Borsi et al, 1972;Fytikas et al, 1976;Ercan et al, 1985;Aydar et al, 2003;Karaoğlu and Helvacı, 2012;Prelevic et al, 2012Prelevic et al, , 2015.…”

mentioning

confidence: 99%

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Alluvial-lacustrine sedimentation and volcaniclastic deposition in an intracontinental tectonic graben: paleoenvironmental evolution of the Neogene Sinanpaşa Basin,west-central Turkey

Akıska¹,

Varol²

2020

Turkish J Earth Sci

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Introduction The Anatolian block of Turkey is located between Eurasian, African, and Arabian plates. As a result of the collision of Africa and Eurasia in the Late Cretaceous, the Anatolian block began to move westward along the dextral North Anatolian Fault System (NAFS) and the sinistral East Anatolian Fault System (EAFS) (McKenzie, 1972; Dewey et al., 1986). This resulted in E-W compression and N-S extension in West Anatolia (Şengör and Yılmaz, 1981). The NAFS and EAFS are the main tectonic features of the Anatolian plate in its escape to the WSW. In addition, there are secondary fault systems extending from the NAFS, deforming the Anatolian plate and dividing it into smaller blocks (Figure 1). The ASFS, located in the western part of Sinanpaşa Basin, studied here, is characterized by a series of grabens and horsts with sets of oblique-slip normal faults controlling the block margins (Koçyiğit and Deveci, 2005). The compressional and extensional tectonics in West Anatolia had led in the Cenozoic to the development of basins bounded by numerous normal faults (Şengör and

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Section: Sedimentary Paleoenvironmentmentioning

confidence: 54%

mentioning

confidence: 99%

Alluvial-lacustrine sedimentation and volcaniclastic deposition in an intracontinental tectonic graben: paleoenvironmental evolution of the Neogene Sinanpaşa Basin,west-central Turkey

Akıska¹,

Varol²

2020

Turkish J Earth Sci

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“…In other cases, we introduce new terminology such as syn-intrusive surface (SyInS), post-degradational surface (PoDgS) and post-burial surface (PoBuS). Further work is necessary to understand how the stratigraphic units of buried volcanic systems correlate with general models of volcanic stratigraphy proposed from outcropping and modern volcanoes [22,[62][63][64][65][66][67]. Table 1 shows the characteristics of the stratigraphic surfaces and their correlative magmatic sequences and stages in the MVS.…”

Section: Syinsmentioning

confidence: 99%

Stratigraphy of Architectural Elements of a Buried Monogenetic Volcanic System

Bischoff¹,

Nicol²,

Cole³

et al. 2019

Preprint

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Large volumes of magma emplaced and deposited within sedimentary basins can have an impact on the architecture and geological evolution of these basins. Over the last decade, continuous improvement in techniques such as seismic volcano-stratigraphy and 3D visualisation of igneous bodies has helped increase knowledge about the architecture of volcanic systems buried in sedimentary basins. Here, we present the complete architecture of the Maahunui Volcanic System (MVS), a middle Miocene monogenetic volcanic field now buried in the offshore Canterbury Basin, South Island of New Zealand. We show the location, geometry, size, and stratigraphic relationships between 25 main intrusive, extrusive and sedimentary architectural elements, in a comprehensive volcano-stratigraphic framework that explains the evolution of the MVS from emplacement to complete burial in the host sedimentary basin. The plumbing system of the MVS comprises saucer-shaped sills, dikes and sill swarms, minor stocks and laccoliths, and pre-eruptive strata deformed by intrusions. The eruptive and associated sedimentary architectural elements define the morphology of volcanoes in the MVS, which comprise deep-water equivalents of crater and cone-type volcanoes. After volcanism ceased, the process of degradation and burial of volcanic edifices formed sedimentary architectural elements such as inter-cone plains, epiclastic plumes, and canyons. Understanding the relationships between these diverse architectural elements allows us to reconstruct the complete architecture of the MVS, including its shallow (<3 km) plumbing system, the morphology of the volcanoes, and their impact in the host sedimentary basin during their burial. Insights from the architecture of the MVS can be used to explore for geoenergy resources such as oil, gas and geothermal energy in buried and active monogenetic volcanic systems elsewhere.

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Syn-eruptive/inter-eruptive relationships in Late Neoproterozoic volcano-sedimentary deposits of the Hamid area, North Eastern Desert, Egypt

Khalaf

2013

Bull Volcanol

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Growth, destruction and volcanic facies architecture of three volcanic centres in the Miocene Uşak–Güre basin, western Turkey: Subaqueous–subaerial volcanism in a lacustrine setting

Cited by 16 publications

References 65 publications

Alluvial-lacustrine sedimentation and volcaniclastic deposition in an intracontinental tectonic graben: paleoenvironmental evolution of the Neogene Sinanpaşa Basin,west-central Turkey

Alluvial-lacustrine sedimentation and volcaniclastic deposition in an intracontinental tectonic graben: paleoenvironmental evolution of the Neogene Sinanpaşa Basin,west-central Turkey

Stratigraphy of Architectural Elements of a Buried Monogenetic Volcanic System

Syn-eruptive/inter-eruptive relationships in Late Neoproterozoic volcano-sedimentary deposits of the Hamid area, North Eastern Desert, Egypt

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