The kinematic and exhumational evolution of the Lesser Himalayan (LH) of Northwest India remains a topic of debate; the resolution of which may provide insight into the relationship between the weathering of chemically ...

Despite advances in understanding the structural development of magma-poor rift margins, the temporal and thermal evolution of lithospheric hyperextension during rifting remains poorly understood. In contrast to classic ...

Following the breakup of the L-Chondrite Parent Body in the Mid-Ordovician, the Earth experienced a drastic increase in the number of meteorite impacts. This event, the Ordovician Meteorite Event (OME), has been confirmed ...