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Dergiler / Turkish Journal of Earth Sciences / 2013 / Cilt: 22 - Sayı: 5

Central Anatolian Plateau, Turkey: incision and paleoaltimetry recorded from volcanic rocks

Erkan AYDAR
H. Evren ÇUBUKÇU
Erdal ŞEN
Lütfiye AKIN
Sayfa
739–746
Yayın Tarihi
2013-05-01
DOI
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⚡ TL;DR(1 Cümlede Hızlı Çıkarım)

Between 5 and 2.5 Ma, the incision rate is computed as 0.12 mm/year, whereas, in the last 2.5 Ma, the incision rate slowed down to 0.04 mm/year.

📌 3 Maddede Bu Makale

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Amaç & Hipotez:The erosion/incision patterns of radiometrically well-constrained volcanic rocks provide excellent markers for revealing the landscape evolution.
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Temel Bulgular & Veri:The Central Anatolian High Plateau represents an uplifted area that reaches up to 1500 m above sea level and includes the Cappadocian Volcanic Province (CVP).
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Sonuç & Katkı:Between 5 and 2.5 Ma, the incision rate is computed as 0.12 mm/year, whereas, in the last 2.5 Ma, the incision rate slowed down to 0.04 mm/year.
🔬Tür:Araştırma Makalesi
📍Kapsam:Genişletilmiş Akademik Örneklem
⚙️Değişkenler:Key words: Cappadocia · incision · uplift

Özet

The erosion/incision patterns of radiometrically well-constrained volcanic rocks provide excellent markers for revealing the landscape evolution. The Central Anatolian High Plateau represents an uplifted area that reaches up to 1500 m above sea level and includes the Cappadocian Volcanic Province (CVP). The CVP is composed of horizontally emplaced Neogene-Quaternary ignimbrites intercalated with lava flows and epiclastic continental sediments. River incision rates have been calculated using the morphological/paleoaltimetric features of radiometrically well-constrained volcanic units in the area. Starting from 10 Ma until 5 Ma, there was no major erosion or incision. The morphology, uplift rate, and incision rates of the CVP reveal that the onset of uplift is post 8 Ma and incision started after 5 Ma. Between 5 and 2.5 Ma, the incision rate is computed as 0.12 mm/year, whereas, in the last 2.5 Ma, the incision rate slowed down to 0.04 mm/year.

Abstract

The erosion/incision patterns of radiometrically well-constrained volcanic rocks provide excellent markers for revealing the landscape evolution. The Central Anatolian High Plateau represents an uplifted area that reaches up to 1500 m above sea level and includes the Cappadocian Volcanic Province (CVP). The CVP is composed of horizontally emplaced Neogene-Quaternary ignimbrites intercalated with lava flows and epiclastic continental sediments. River incision rates have been calculated using the morphological/paleoaltimetric features of radiometrically well-constrained volcanic units in the area. Starting from 10 Ma until 5 Ma, there was no major erosion or incision. The morphology, uplift rate, and incision rates of the CVP reveal that the onset of uplift is post 8 Ma and incision started after 5 Ma. Between 5 and 2.5 Ma, the incision rate is computed as 0.12 mm/year, whereas, in the last 2.5 Ma, the incision rate slowed down to 0.04 mm/year.

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Bu Makaleye Atıf Yap

AYDAR, E., ÇUBUKÇU, H. E., ŞEN, E., AKIN, L. (2013). Central Anatolian Plateau, Turkey: incision and paleoaltimetry recorded from volcanic rocks. Turkish Journal of Earth Sciences, Cilt: 22 - Sayı: 5, 739–746. https://ajindex.com/articles/209928

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Kaynakça (11)

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