4.4 Article

The Toba Caldera Complex

Journal

QUATERNARY INTERNATIONAL
Volume 258, Issue -, Pages 5-18

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.quaint.2011.09.025

Keywords

-

Ask authors/readers for more resources

The Toba Caldera in Indonesia is one of the most remarkable volcanic features formed during Quaternary geologic time. Its rich history of research for over a century has yielded important information on the physical volcanology of silicic calderas and super-eruptions, geochemical evolution of silicic magma bodies, and geophysical imaging of active sub-volcanic systems. During the past 13 my, the Toba area has erupted intermediate composition lavas, followed by intermediate pyroclastics, three quartz-bearing silicic tuffs, and most recently, intermediate to silicic lavas. This pattern represents the incremental assembly and periodic eruption of a crustal magma body of batholithic proportions. The apparent migration of activity to the west, may have implications for the next? Toba super-eruption. (C) 2011 Elsevier Ltd and INQUA. All rights reserved.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.4
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available