The Yalvaç Basin is a sedimentary basin located in the northern tip of the Isparta Angle.[1]: 369–70 It generally runs from northwest to southeast and is about 55 km long and 15 km wide.[1]: 370 Lake Beyşehir occupies its southern part, while at its northwestern end is the village of Yarıkkaya.[2]: 3.1 To the north, east, and west, the Yalvaç Basin is bounded by mountains, such as the Sultandağları mountains.[1]: 372
The Yalvaç Basin's shape and size have been mostly the same since its formation, either during or shortly before the Middle Miocene, and sedimentary deposition has been occurring here since then.[1]: 395
Stratigraphyedit
The Yalvaç Basin consists of four main geological formations, from oldest to youngest: the Bağkonak Formation, the Yarıkkaya Formation, the Göksöğüt Formation, and the Kırkbaş Formation.[1]: 372 Their total thickness is about 800 m.[1]: 372 Below these are basement rocks of diverse origin including ophiolites, metamorphic rocks from the Afyon zone, and non-metamorphic rocks that originally came from the Tauride fold and thrust belt and were thrust here in Cretaceous through Eocene times.[1]: 395
The Bağkonak Formation, the oldest formation in the basin, unconformably overlies pre-Neogene basement rocks.[1]: 373, 5 It is especially well exposed south of Yalvaç, near Özbayat and Bağkonak.[1]: 373, 5 It is about 250 m thick and mostly consists of "continental red clastics with dominantly conglomerates at the bottom and intercalating sandstone and sandy-mudstone towards the upper levels".[1]: 373 It was probably formed by sedimentary deposits in river deltas and alluvial fans along the border between the Yalvaç Basin and the Sultandağları mountains.[1]: 375 No fossils have been found in the Bağkonak Formation.[1]: 375
The Yarıkkaya Formation unconformably overlies the pre-Neogene basement rocks in the north and conformably overlies the Bağkonak Formation in the south.[1]: 376 Its composition ranges from "coarse, sub-rounded, poorly sorted, grain-supported conglomerate" at the bottom to sandstone in the middle to coarser conglomerate at the top.[1]: 375 The lower parts were likely formed as river deposits; towards the central part of the basin, "fine mud/clay, marly limestone, and tufa deposits" represent shallow lake deposits.[1]: 378 Lignite seams represent deposition from swamp environments.[1]: 378 Fossils include freshwater gastropod species like Planorbis and Limnea found in mudstone and claystone deposits, and vertebrates like rodents and hamsters found in upper levels deposited from lake environments.[1]: 378 Various ages have been estimated for this formation; Yağmurlu suggested a Middle Miocene date based on the gastropod fossils, while Saraç proposed an Early-Middle Miocene date based on the vertebrate fossils.[1]: 378
The Göksöğüt Formation overlies the Yarıkkaya Formation, unconformably in the north and conformably in the south.[1]: 376 At the bottom, it consists of "banded, highly porous brownish limestone", and further upward it coarsens into conglomerate.[1]: 378–9 The overall formation is at least 150 m thick.[1]: 379 It is especially exposed around Ayvalı and north of Körküler.[1]: 379 The coarsening of deposits from bottom to top is interpreted by Koç et al. as sedimentary infilling of a lake basin by "high-energy" river systems.[1]: 379 Fossils of the gastropods Planorbis and Limnea have been found in the marl and claystone levels of the Göksöğüt Formation, although Yağmurlu said these were "endemic" and cautioned against using them to date the formation.[1]: 379
The Kırkbaş Formation unconformably overlies the Göksöğüt Formation and mainly consists of "reddish, poorly consolidated conglomerate, sandstone, and mudstone alternations".[1]: 380 It is itself overlain by Quaternary alluvial deposits.[1]: 380 It is especially visible around Kırkbaş and east of Terziler.[1]: 380 Around Tokmacık, Hipparion and Mastodon fossils have been found, indicating that the Kırkbaş Formation dates to the Pliocene period.[1]: 380
Faultsedit
The edges of the Yalvaç Basin are marked by various large-scale normal faults.[1]: 380 Within the basin, there are many medium-sized faults with displacements of a few centimeters to a few meters.[1]: 380 The primary fault directions are northwest–southeast and northeast–southwest, indicating that the local tectonics are controlled by two main "zones of weakness".[1]: 381
The most prominent fault zone in the area is the Yarıkkaya Fault Zone.[1]: 381 It runs west toward the Karacaören Fault and east toward the Sultandağları mountains, where it dies out.[1]: 381 Another zone is the Çakırçal Fault Zone, which goes northwest–southeast for over 15 km and is itself interrupted by the eastern part of the Yarıkkaya Fault Zone.[1]: 382 Then there is the Sağır Fault Zone, which forms an 18 km-long valley running northwest–southeast west of Sağır.[1]: 382 It is also cut up by the Yarıkkaya Fault Zone, as well as by the northeast–southwest-trending Kumdanlı Fault Zone.[1]: 382 The Kumdanlı Fault Zone itself runs for about 20 km, from Mısırlı in the northeast to south of Aşağıtırtar in the southwest before disappearing into Lake Hoyran.[1]: 382 Its northeastern end disappears into the Yalvaç Basin's sedimentary infill.[1]: 383 Another fault zone is the northeast-southwest Yaka Fault zone, which is about 6 km wide and over 20 km long.[1]: 384 It runs from south of Gelendost at its southwestern end to near Madenli in the northeast.[1]: 384 The Yaka Fault Zone controls the southern margin of the Yalvaç Basin and separates the Yarıkkaya Formation from the underlying basement rocks.[1]: 384
Referencesedit
^ abcdefghijklmnopqrstuvwxyzaaabacadaeafagahaiajakalamanaoKoç, Ayten; Kaymakci, Nuretdin; van Hinsbergen, Douwe J.J.; Vissers, Reinoud L.M. (2014). "A Miocene onset of the modern extensional regime in the Isparta Angle: constraints from the Yalvaç Basin (southwest Turkey)". International Journal of Earth Sciences. 101 (1): 369–98. doi:10.1007/s00531-014-1100-z. Retrieved 28 March 2023.
^Koçyiğit, Ali; Gürboğa, Şule; Kalafat, Doğan (2012). "Nature and onset age of neotectonic regime in the northern core of Isparta Angle, SW Turkey". Geodinamica Acta. 25 (1–2): 52–85. doi:10.1080/09853111.2013.839126. Retrieved 15 February 2023.
January 01, 1970
yalvaç, basin, sedimentary, basin, turkey, around, lake, beyşehir, present, town, yalvaç, lies, within, geological, region, known, isparta, angle, existed, since, miocene, times, contents, general, description, stratigraphy, faults, referencesgeneral, descript. The Yalvac Basin is a sedimentary basin in Turkey around Lake Beysehir and the present day town of Yalvac It lies within the geological region known as the Isparta Angle It has existed since Miocene times Contents 1 General description 2 Stratigraphy 3 Faults 4 ReferencesGeneral description editThe Yalvac Basin is a sedimentary basin located in the northern tip of the Isparta Angle 1 369 70 It generally runs from northwest to southeast and is about 55 km long and 15 km wide 1 370 Lake Beysehir occupies its southern part while at its northwestern end is the village of Yarikkaya 2 3 1 To the north east and west the Yalvac Basin is bounded by mountains such as the Sultandaglari mountains 1 372 The Yalvac Basin s shape and size have been mostly the same since its formation either during or shortly before the Middle Miocene and sedimentary deposition has been occurring here since then 1 395 Stratigraphy editThe Yalvac Basin consists of four main geological formations from oldest to youngest the Bagkonak Formation the Yarikkaya Formation the Goksogut Formation and the Kirkbas Formation 1 372 Their total thickness is about 800 m 1 372 Below these are basement rocks of diverse origin including ophiolites metamorphic rocks from the Afyon zone and non metamorphic rocks that originally came from the Tauride fold and thrust belt and were thrust here in Cretaceous through Eocene times 1 395 The Bagkonak Formation the oldest formation in the basin unconformably overlies pre Neogene basement rocks 1 373 5 It is especially well exposed south of Yalvac near Ozbayat and Bagkonak 1 373 5 It is about 250 m thick and mostly consists of continental red clastics with dominantly conglomerates at the bottom and intercalating sandstone and sandy mudstone towards the upper levels 1 373 It was probably formed by sedimentary deposits in river deltas and alluvial fans along the border between the Yalvac Basin and the Sultandaglari mountains 1 375 No fossils have been found in the Bagkonak Formation 1 375 The Yarikkaya Formation unconformably overlies the pre Neogene basement rocks in the north and conformably overlies the Bagkonak Formation in the south 1 376 Its composition ranges from coarse sub rounded poorly sorted grain supported conglomerate at the bottom to sandstone in the middle to coarser conglomerate at the top 1 375 The lower parts were likely formed as river deposits towards the central part of the basin fine mud clay marly limestone and tufa deposits represent shallow lake deposits 1 378 Lignite seams represent deposition from swamp environments 1 378 Fossils include freshwater gastropod species like Planorbis and Limnea found in mudstone and claystone deposits and vertebrates like rodents and hamsters found in upper levels deposited from lake environments 1 378 Various ages have been estimated for this formation Yagmurlu suggested a Middle Miocene date based on the gastropod fossils while Sarac proposed an Early Middle Miocene date based on the vertebrate fossils 1 378 The Goksogut Formation overlies the Yarikkaya Formation unconformably in the north and conformably in the south 1 376 At the bottom it consists of banded highly porous brownish limestone and further upward it coarsens into conglomerate 1 378 9 The overall formation is at least 150 m thick 1 379 It is especially exposed around Ayvali and north of Korkuler 1 379 The coarsening of deposits from bottom to top is interpreted by Koc et al as sedimentary infilling of a lake basin by high energy river systems 1 379 Fossils of the gastropods Planorbis and Limnea have been found in the marl and claystone levels of the Goksogut Formation although Yagmurlu said these were endemic and cautioned against using them to date the formation 1 379 The Kirkbas Formation unconformably overlies the Goksogut Formation and mainly consists of reddish poorly consolidated conglomerate sandstone and mudstone alternations 1 380 It is itself overlain by Quaternary alluvial deposits 1 380 It is especially visible around Kirkbas and east of Terziler 1 380 Around Tokmacik Hipparion and Mastodon fossils have been found indicating that the Kirkbas Formation dates to the Pliocene period 1 380 Faults editThe edges of the Yalvac Basin are marked by various large scale normal faults 1 380 Within the basin there are many medium sized faults with displacements of a few centimeters to a few meters 1 380 The primary fault directions are northwest southeast and northeast southwest indicating that the local tectonics are controlled by two main zones of weakness 1 381 The most prominent fault zone in the area is the Yarikkaya Fault Zone 1 381 It runs west toward the Karacaoren Fault and east toward the Sultandaglari mountains where it dies out 1 381 Another zone is the Cakircal Fault Zone which goes northwest southeast for over 15 km and is itself interrupted by the eastern part of the Yarikkaya Fault Zone 1 382 Then there is the Sagir Fault Zone which forms an 18 km long valley running northwest southeast west of Sagir 1 382 It is also cut up by the Yarikkaya Fault Zone as well as by the northeast southwest trending Kumdanli Fault Zone 1 382 The Kumdanli Fault Zone itself runs for about 20 km from Misirli in the northeast to south of Asagitirtar in the southwest before disappearing into Lake Hoyran 1 382 Its northeastern end disappears into the Yalvac Basin s sedimentary infill 1 383 Another fault zone is the northeast southwest Yaka Fault zone which is about 6 km wide and over 20 km long 1 384 It runs from south of Gelendost at its southwestern end to near Madenli in the northeast 1 384 The Yaka Fault Zone controls the southern margin of the Yalvac Basin and separates the Yarikkaya Formation from the underlying basement rocks 1 384 References edit a b c d e f g h i j k l m n o p q r s t u v w x y z aa ab ac ad ae af ag ah ai aj ak al am an ao Koc Ayten Kaymakci Nuretdin van Hinsbergen Douwe J J Vissers Reinoud L M 2014 A Miocene onset of the modern extensional regime in the Isparta Angle constraints from the Yalvac Basin southwest Turkey International Journal of Earth Sciences 101 1 369 98 doi 10 1007 s00531 014 1100 z Retrieved 28 March 2023 Kocyigit Ali Gurboga Sule Kalafat Dogan 2012 Nature and onset age of neotectonic regime in the northern core of Isparta Angle SW Turkey Geodinamica Acta 25 1 2 52 85 doi 10 1080 09853111 2013 839126 Retrieved 15 February 2023 Retrieved from https en wikipedia org w index php title Yalvac Basin amp oldid 1188158204, wikipedia, wiki, book, books, library,
