Measurement of tectonic surface uplift rate in a young collisional mountain belt

Lon D. Abbott; Eli A. Silver; Robert S. Anderson; Randall Smith; James C. lngle; Stanley A. Kling; David Haig; Eric Small; Joseph Galewsky; William Sliter

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Measurement of tectonic surface uplift rate in a young collisional mountain belt

机译：年轻的碰撞山带构造面抬升速率的测量

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Measurement of the rate of tectonically driven surface uplift is crucial to a complete understanding of mountain building dynamics. The lack of a suitable rock record typically prevents determination of this quantity, but the unusual geology of Papua New Guinea's Flnlsterre mountains makes measurement of this rate possible. The tectonic surface uplift rate at the Finisterre range is 0.8-2.1 mm yr~(-1), approximately that expected to arise from crustal thickening.

机译：测量构造驱动的表面隆起的速率对于全面了解山区建筑动力学至关重要。缺乏合适的岩石记录通常无法确定该数量，但是巴布亚新几内亚的Flnlsterre山区异常的地质状况使得该速率的测量成为可能。 Finisterre范围内的构造表面抬升速率为0.8-2.1 mm yr〜（-1），大约是地壳增厚所预期的。

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《Nature》 |1997年第6616期|p.501-507|共7页
作者
Lon D. Abbott; Eli A. Silver; Robert S. Anderson; Randall Smith; James C. lngle; Stanley A. Kling; David Haig; Eric Small; Joseph Galewsky; William Sliter;
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收录信息美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
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正文语种 eng
中图分类自然科学总论;
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Measurement of tectonic surface uplift rate in a young collisional mountain belt

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