The Infona portal uses cookies, i.e. strings of text saved by a browser on the user's device. The portal can access those files and use them to remember the user's data, such as their chosen settings (screen view, interface language, etc.), or their login data. By using the Infona portal the user accepts automatic saving and using this information for portal operation purposes. More information on the subject can be found in the Privacy Policy and Terms of Service. By closing this window the user confirms that they have read the information on cookie usage, and they accept the privacy policy and the way cookies are used by the portal. You can change the cookie settings in your browser.
The evolution of the magmatic arc formed along the Asian margin of Neo-Tethys is a key to understand India–Asia convergence. In contrast to the well studied trans-Himalayan magmatic rocks in Tibet, the southeast extension of the arc is still poorly documented in Myanmar, where it is largely buried by sedimentary rocks. This study investigates the magmatic evolution of the western Myanmar arc and the...
Before the continental collision of India with Asia, northward subduction of the Tethyan oceanic lithosphere beneath South Asia resulted in widespread arc magmatism in the Lhasa terrane of southern Tibet from Early Jurassic to Eocene time. The detailed magmatic history of this Transhimalayan arc system, however, remains unclear. Here we report in-situ detrital zircon U–Pb and Hf isotopic analyses...
Set the date range to filter the displayed results. You can set a starting date, ending date or both. You can enter the dates manually or choose them from the calendar.