A tectonically controlled alluvial fan which developed into a marine fan-delta at a complex triple junction: Miocene Gildirli Formation of the Adana Basin, Turkey
- 1 December 1992
- journal article
- Published by Elsevier in Sedimentary Geology
- Vol. 81 (3-4) , 243-252
- https://doi.org/10.1016/0037-0738(92)90073-z
Abstract
No abstract availableKeywords
This publication has 9 references indexed in Scilit:
- Ordovician alluvial fan to marine shelf transition in SW Sardinia, Western Mediterranean Sea: tectonically (“Sardic phase”) influenced clastic sedimentationSedimentary Geology, 1991
- Architectural-element analysis: A new method of facies analysis applied to fluvial depositsEarth-Science Reviews, 1985
- Structure and deformation history of the Bitlis suture near Lake Hazar, southeastern TurkeyGSA Bulletin, 1985
- Active tectonics of the Alpine--Himalayan Belt between western Turkey and PakistanGeophysical Journal International, 1984
- Alluvial-fan sedimentation of the Cutler Formation (Permo-Pennsylvanian) near Gateway, ColoradoGSA Bulletin, 1984
- Tethyan evolution of Turkey: A plate tectonic approachTectonophysics, 1981
- The North Anatolian transform fault: its age, offset and tectonic significanceJournal of the Geological Society, 1979
- Early Tertiary sedimentation in the western Uinta Basin, UtahGSA Bulletin, 1976
- GEOLOGY OF ALLUVIAL FANS IN SEMIARID REGIONSGSA Bulletin, 1954