Knowing the original size of Greater India is a fundamental parameter to quantify the amount
of continental lithosphere that was subducted to help form the Tibetan Plateau and to …

Greater India comprises a part of the Indian plate that subducted under Asia to help form the
Tibetan Plateau. Defining the size of the Greater India is thus a key constraint to model the …

The Río Chico Group in the San Jorge Basin of central Patagonia (Argentina) preserves
some of South America's most significant Paleogene records of biotic and climatic change …

Abstract The Late Cretaceous and Paleogene sediments from the Tethyan Himalaya can
provide paleomagnetic constraints on the pre-collision size of Greater India. However …

The Sangdanlin section in southern Tibet represents a geologic Rosetta stone to constrain
the initiation of the India–Asia collision from its sedimentary and paleomagnetic records …

We present a new, automated system based on a three‐axis superconducting
magnetometer and a custom‐made coil designed to experiment on cylindrical specimens …

Hainan Island lies near the Red River Fault, a prominent tectonic feature produced by the
India‐Asia collision. There, we carried out a geochronologic and paleomagnetic study on …

Studies on the paleogeographic evolution of the Southern Qiangtang terrane, as an integral
component of the Cimmerian continent, are essential for understanding the geodynamic …

Impact melt breccias from the Rochechouart (France) meteorite crater possess
paleomagnetic directions with both normal and reverse polarities, raising the question …

We carried out an integrated rock magnetic and paleomagnetic study of the∼ 36 Ma
Mistastin Lake (Labrador, Canada) meteorite impact structure in order to investigate whether …