Miocene faulting at plate tectonic velocity in the Himalaya of central Nepal

被引:150
作者
Kohn, MJ [1 ]
Wieland, MS
Parkinson, CD
Upreti, BN
机构
[1] Univ S Carolina, Dept Geol Sci, Columbia, SC 29208 USA
[2] Univ New Orleans, Dept Geol & Geophys, New Orleans, LA 70148 USA
[3] Tribhuvan Univ, Dept Geol, Kathmandu, Nepal
基金
美国国家科学基金会;
关键词
Himalaya; geochronology; monazite; metamorphism; melting;
D O I
10.1016/j.epsl.2004.10.007
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Combination of geochemical zoning in metamorphic garnet and monazite plus in situ Th-Pb isotopic dating of monazite yields P-T conditions, ages and convergence rates for the Main Central Thrust (MCT) and affiliated faults in central Nepal. Inferred rates were 1.5+/-0.9 cm/yr (Langtang Thrust, similar to19 Ma), 2.2+/-0.7 cm/yr (Main Central Thrust, similar to15 Ma) and 7+/-3 cm/yr (Ramgarh Thrust, similar to10 Ma). The lower values are similar to modern convergence rates across the Himalaya, but the Ramgarh Thrust may have briefly absorbed all Indo-Asian convergence at similar to10 Ma. when foreland and marine sedimentation rates markedly increased, and at least one major strike slip fault in Tibet experienced a hiatus in movement. Variable rates of convergence across the Himalaya on Myr timescales imply Myr variations in strain rates throughout all components of the Indo-Asian orogen. (C) 2004 Elsevier B.V. All rights reserved.
引用
收藏
页码:299 / 310
页数:12
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