中新世安纳托利亚高原内部(t rkiye)与现代山地边缘的表面隆起解耦

IF 4.8 1区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
Maud J.M. Meijers , Tamás Mikes , Bora Rojay , Erkan Aydar , H. Evren Çubukçu , Thomas Wagner , Tina Lüdecke , Emilija Krsnik , Jens Fiebig , Andreas Mulch
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引用次数: 0

摘要

中安纳托利亚高原(CAP)形成了土耳其-伊朗高原的西部,自约41 Ma以来大部分地区保持在海平面以上。然而,目前的CAP地形主要是在晚中新世以来发展起来的,平均海拔约为1.0-1.5 km,北部和南部的山区边缘局部高峰海拔超过3 km。为了明确地表隆起的模式,我们利用稳定同位素古高程和双团块同位素古温标法对CAP和附近沿海地区的土壤碳酸盐进行了近10 Ma的古高程估算。从爱琴海-安纳托利亚地区收集的数据显示,中新世之后,土壤碳酸盐的δ18O值持续增加,以响应区域干旱化的增加。古海拔测量和双团块同位素结果表明,自10 Ma以来,CAP一直处于比现代沿海地区更高的海拔。在约8 ~ 6 Ma时,我们的精确古高程估计表明存在约1.5 km高的地形障碍。然而,南缘和北缘的Tauride山和Pontide山的地表隆升晚于CAP的地表隆升。因此,晚中新世CAP和其山地边缘的地表隆升是分离的,这意味着它们的非同步形成具有不同的地球动力驱动。考虑到Tauride山脉在7 Ma之后出现在地中海,我们记录了晚中新世以来南部高原边缘的向外生长。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Miocene decoupling of surface uplift of the Central Anatolian Plateau interior (Türkiye) and its modern mountainous margins
The Central Anatolian Plateau (CAP) forms the western portion of the Turkish-Iranian plateau and has mostly remained above sea level since ca. 41 Ma. However, the current topography of the CAP has predominantly developed since the Late Miocene, with mean elevations of ca. 1.0–1.5 km and northern and southern mountainous margins with peak elevations that locally exceed 3 km. To clarify patterns of surface uplift, we present paleoelevation estimates for the past 10 Ma by applying stable isotope paleoaltimetry on soil carbonates from the CAP and nearby coastal regions, as well as dual clumped isotope paleothermometry.
The compiled datasets from the Aegean-Anatolian region display a sustained increase in δ18O values of soil carbonates after the Miocene, in response to increased regional aridification. Our paleoaltimetry and dual clumped isotope results indicate that the CAP has been at higher elevations than the modern coastal regions since 10 Ma. By ca. 8 − 6 Ma, our refined paleoaltimetry estimates indicate the presence of a ca. 1.5 km-high orographic barrier. However, surface uplift of the Tauride and Pontide mountains on the southern and northern plateau margin postdate surface uplift of the CAP. Therefore, surface uplift of the CAP and its mountainous margins were decoupled during the Late Miocene, implying distinct geodynamic drivers for their asynchronous formation. Given that the Tauride Mts. emerged from the Mediterranean after 7 Ma, we document outward growth of the southern plateau margin since the Late Miocene.
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来源期刊
Earth and Planetary Science Letters
Earth and Planetary Science Letters 地学-地球化学与地球物理
CiteScore
10.30
自引率
5.70%
发文量
475
审稿时长
2.8 months
期刊介绍: Earth and Planetary Science Letters (EPSL) is a leading journal for researchers across the entire Earth and planetary sciences community. It publishes concise, exciting, high-impact articles ("Letters") of broad interest. Its focus is on physical and chemical processes, the evolution and general properties of the Earth and planets - from their deep interiors to their atmospheres. EPSL also includes a Frontiers section, featuring invited high-profile synthesis articles by leading experts on timely topics to bring cutting-edge research to the wider community.
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