Rise of the Andes.
نویسندگان
چکیده
The surface uplift of mountain belts is generally assumed to reflect progressive shortening and crustal thickening, leading to their gradual rise. Recent studies of the Andes indicate that their elevation remained relatively stable for long periods (tens of millions of years), separated by rapid (1 to 4 million years) changes of 1.5 kilometers or more. Periodic punctuated surface uplift of mountain belts probably reflects the rapid removal of unstable, dense lower lithosphere after long-term thickening of the crust and lithospheric mantle.
منابع مشابه
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ورودعنوان ژورنال:
- Science
دوره 320 5881 شماره
صفحات -
تاریخ انتشار 2008