Abstract Otavi Group is a 1.5–3.5-km-thick epicontinental marine carbonate succession of
Neoproterozoic age, exposed in an 800-km-long Ediacaran− Cambrian fold belt that rims …

Flood volcanic provinces are assumed generally to consist exclusively of thick lavas and
shallow intrusive rocks (mostly sills), with any pyroclastic rocks limited to silicic compositions …

Authoritative, accessible, and updated introduction to sedimentary rocks for undergraduate
students Sedimentary Petrology provides readers with a concise account of sedimentary …

The volcanic rocks of the Lower Cretaceous Paraná-Etendeka Igneous Province, in Brazil,
are grouped in the Serra Geral Group. The province can be chemically divided into low-TiO …

The internal architecture of the immense volumes of eruptive products in Continental Flood
Basalt Provinces (CFBPs) provides vital clues, through the constraint of a chrono …

A fast and effective method has been developed to measure total optical porosity (TOP) of
blue resin-impregnated thin sections. This utilises a macro file (jPOR. txt) for ImageJ, which …

Based on four decades of research by Professor Andrew Goudie, this volume provides a
state-of-the-art synthesis of our understanding of desert geomorphology. It presents a truly …

Gondwana was an enormous supertarrane. At its peak, it represented a landmass of about
100× 10 6 km 2 in size, corresponding to approximately 64% of all land areas today …

The correlation between large igneous provinces (LIPs), extinction events, and rapid climate
change suggests that volcanism can have a detrimental impact on Earth surface conditions …

The sedimentary record of aeolian sand systems extends from the A rchean to the Q
uaternary, yet current understanding of aeolian sedimentary processes and product remains …