Konya Karapinar obruks (sinkholes) of Turkey

Publication:
Konya Karapinar obruks (sinkholes) of Turkey

dc.contributor.author	Erosykay, Okan
dc.contributor.author	Gültekin, Günay
dc.contributor.author	Corekcioglu, I.
dc.contributor.author	Ovul, G.
dc.contributor.authorID	289095	tr_TR
dc.date.accessioned	2018-07-30T06:42:42Z
dc.date.available	2018-07-30T06:42:42Z
dc.date.issued	2010
dc.description.abstract	Konya plain in Central Anatolia features various unique karstic formations from different ages. The most peculiar of these formations are the obruks, which are mainly found within the lacustrine limestone of Neogene age. The unconfined groundwater in the region outcrops in the form of obruk lakes. The Neogene formations at the upper part and the basement limestones are hydraulically linked. The Neogene formation is more porous because of cavities, and the pervious nature of the basement is due to karst conduits. The obruks have been formed by the combined effects of the carbonates, structures, karstification, and the tectonic history of the area.	tr_TR
dc.identifier.isbn	978-3-642-12485-3
dc.identifier.issn	2199-9155
dc.identifier.uri	https://doi.org/10.1007/978-3-642-12486-0_57
dc.identifier.uri	https://hdl.handle.net/11413/2393
dc.identifier.wos	395214400057
dc.language.iso	en
dc.publisher	Springer International Publishing Ag, Gewerbestrasse 11, Cham, Ch-6330, Switzerland
dc.relation	Advances in Research in Karst Media	tr_TR
dc.title	Konya Karapinar obruks (sinkholes) of Turkey	tr_TR
dc.type	Article
dspace.entity.type	Publication
local.indexed.at	WOS