SwePub
Sök i LIBRIS databas

  Extended search

id:"swepub:oai:DiVA.org:su-147904"
 

Search: id:"swepub:oai:DiVA.org:su-147904" > South Menderes Mono...

  • 1 of 1
  • Previous record
  • Next record
  •    To hitlist

South Menderes Monocline : Low-temperature thermochronology constrains role of crustal extension in structural evolution of southwest Turkey

Ring, Uwe (author)
Stockholms universitet,Institutionen för geologiska vetenskaper
Gessner, Klaus (author)
Thomson, Stuart N. (author)
 (creator_code:org_t)
Elsevier BV, 2017
2017
English.
In: Tectonophysics. - : Elsevier BV. - 0040-1951 .- 1879-3266. ; 712, s. 455-463
  • Journal article (peer-reviewed)
Abstract Subject headings
Close  
  • We report apatite and zircon fission-track data across the contact zones between the Menderes nappes, the Cycladic blueschist unit, and the Oren nappe, in the Anatolide belt of southwest Turkey. These data resolve previous debate on the deformation history of these Cretaceous to Eocene nappe contacts, including whether they were reactivated during late Oligocene to Miocene crustal extension. Apatite fission-track ages range from 18 to 28 Ma in the Menderes nappes, and 31 to 42 Ma in the Oren nappe. Zircon fission-track ages are 29 to 31 Ma in the Menderes nappes, 30 to 33 Ma in the Cycladic blueschist unit, and between 93 Ma and 129 Ma in the Oren nappe. The data reveal that the tectonic contacts within the Menderes nappes, and with the overlying Cycladic blueschist unit have been sealed since similar to 35-30 Ma. In the Oren nappe, zircon fission-track ages are distinctly older (with mixed single grain ages between similar to 300 and 75 Ma) reflecting partial to full resetting during late Cretaceous high-pressure metamorphism, The contact between the Cycladic blueschist unit and the Oren nappe shows no significant tectonic movement in the brittle crust after similar to 70 Ma. These data reveal that the nappe boundaries in the southern Menderes Massif have undergone no significant differential offset relative to the Earth's surface since the Oligocene and therefore were not reactivated during late Oligocene to Miocene continental extension. We interpret the steeply dipping portion of the nappe pile in the southern Menderes Massif as a tilted crustal section, which we name the 'South Menderes Monocline'. We speculate this monocline formed by differential uplift in the Miocene, either at the hinge zone of a plateau, or by unloading of the Simav detachment footwall.

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences (hsv//eng)

Keyword

Tectonic contacts
Nappes
Fission-track dating
Extensional sedimentary basins
Menderes Massif
Aegean Sea region

Publication and Content Type

ref (subject category)
art (subject category)

Find in a library

To the university's database

  • 1 of 1
  • Previous record
  • Next record
  •    To hitlist

Find more in SwePub

By the author/editor
Ring, Uwe
Gessner, Klaus
Thomson, Stuart ...
About the subject
NATURAL SCIENCES
NATURAL SCIENCES
and Earth and Relate ...
Articles in the publication
Tectonophysics
By the university
Stockholm University

Search outside SwePub

Kungliga biblioteket hanterar dina personuppgifter i enlighet med EU:s dataskyddsförordning (2018), GDPR. Läs mer om hur det funkar här.
Så här hanterar KB dina uppgifter vid användning av denna tjänst.

 
pil uppåt Close

Copy and save the link in order to return to this view