Unknown

Dataset Information

0

Erosion in southern Tibet shut down at ∼10 Ma due to enhanced rock uplift within the Himalaya.


ABSTRACT: Exhumation of the southern Tibetan plateau margin reflects interplay between surface and lithospheric dynamics within the Himalaya-Tibet orogen. We report thermochronometric data from a 1.2-km elevation transect within granitoids of the eastern Lhasa terrane, southern Tibet, which indicate rapid exhumation exceeding 1 km/Ma from 17-16 to 12-11 Ma followed by very slow exhumation to the present. We hypothesize that these changes in exhumation occurred in response to changes in the loci and rate of rock uplift and the resulting southward shift of the main topographic and drainage divides from within the Lhasa terrane to their current positions within the Himalaya. At ∼17 Ma, steep erosive drainage networks would have flowed across the Himalaya and greater amounts of moisture would have advected into the Lhasa terrane to drive large-scale erosional exhumation. As convergence thickened and widened the Himalaya, the orographic barrier to precipitation in southern Tibet terrane would have strengthened. Previously documented midcrustal duplexing around 10 Ma generated a zone of high rock uplift within the Himalaya. We use numerical simulations as a conceptual tool to highlight how a zone of high rock uplift could have defeated transverse drainage networks, resulting in substantial drainage reorganization. When combined with a strengthening orographic barrier to precipitation, this drainage reorganization would have driven the sharp reduction in exhumation rate we observe in southern Tibet.

SUBMITTER: Tremblay MM 

PROVIDER: S-EPMC4593086 | biostudies-literature | 2015 Sep

REPOSITORIES: biostudies-literature

altmetric image

Publications

Erosion in southern Tibet shut down at ∼10 Ma due to enhanced rock uplift within the Himalaya.

Tremblay Marissa M MM   Fox Matthew M   Schmidt Jennifer L JL   Tripathy-Lang Alka A   Wielicki Matthew M MM   Harrison T Mark TM   Zeitler Peter K PK   Shuster David L DL  

Proceedings of the National Academy of Sciences of the United States of America 20150914 39


Exhumation of the southern Tibetan plateau margin reflects interplay between surface and lithospheric dynamics within the Himalaya-Tibet orogen. We report thermochronometric data from a 1.2-km elevation transect within granitoids of the eastern Lhasa terrane, southern Tibet, which indicate rapid exhumation exceeding 1 km/Ma from 17-16 to 12-11 Ma followed by very slow exhumation to the present. We hypothesize that these changes in exhumation occurred in response to changes in the loci and rate o  ...[more]

Similar Datasets

| S-EPMC7725450 | biostudies-literature
| S-EPMC6367307 | biostudies-literature
| S-EPMC8291530 | biostudies-literature
| S-EPMC4205732 | biostudies-other
| S-EPMC4944177 | biostudies-literature
| S-EPMC7160121 | biostudies-literature
| S-EPMC10963718 | biostudies-literature
| S-EPMC7029067 | biostudies-literature
| S-EPMC5073360 | biostudies-literature
| S-EPMC11337062 | biostudies-literature