Far-field tectonic effects of the Arabia-Eurasia collision and the inception of the North Anatolian Fault system

被引：28

作者：

Albino, Irene ^{[1
]}

Cavazza, William ^{[1
]}

Zattin, Massimiliano ^{[2
]}

Okay, Aral I. ^{[3
]}

Adamia, Shota ^{[4
]}

Sadradze, Nino ^{[5
]}

机构：

[1] Univ Bologna, Dept Biol Geol & Environm Sci, I-40126 Bologna, Italy

[2] Univ Padua, Dept Geosci, I-35131 Padua, Italy

[3] Istanbul Tech Univ, Eurasia Inst Earth Sci, TR-34469 Istanbul, Turkey

[4] Inst Geophys, GE-0193 Tbilisi, Georgia

[5] Inst Geol, GE-0193 Tbilisi, Georgia

来源：

GEOLOGICAL MAGAZINE | 2014年 / 151卷 / 02期

关键词：

fission-track analysis; low-temperature thermochronology; stress transfer; exhumation; WESTERN GREATER CAUCASUS; TRACK ANNEALING KINETICS; SURROUNDING REGIONS; EVOLUTION; CONSTRAINTS; BASIN; LITHOSPHERE; VARIABILITY; DYNAMICS; PLATE;

D O I：

10.1017/S0016756813000952

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

New thermochronological data show that rapid Middle Miocene exhumation occurred synchronously along the Bitlis suture zone and in the southeastern Black Sea region, arguably as a far-field effect of the Arabia-Eurasia indentation. Collision-related strain focused preferentially along the rheological boundary between the multideformed continental lithosphere of northeastern Anatolia and the strong (quasi)oceanic lithosphere of the eastern Black Sea. Deformation in the southeastern Black Sea region ceased in late Middle Miocene time, when coherent westward motion of Anatolia and the corresponding activation of the North and East Anatolian Fault systems mechanically decoupled portions of the foreland from the Arabia-Eurasia collision zone.

引用

页码：372 / 379

页数：8

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