
Miller, and Miller-Bravais indices are the standard where every face on a crystal is given
Miller, and Miller-Bravais indices are the standard where every face on a crystal is given
Preview (opens in a new tab) Not really a CV, more a precis 1969 and
The utility of lithic grains as provenance indicators The composition of terrigenous sandstone is usually
The term neomorphism is reserved for recrystallization of a mineral and its polymorphs to new
Ignimbrite is a rock name. Ignimbrites form primarily from the collapse of eruption columns during
Glauconite – an important stratigraphic and paleoenvironmental indicator Glauconite is one of the most recognizable
Two important contributors to bioclastic limestones – foram tests and skeletal sponge spicules Foraminifera
Bryozoa – are a complex but important group of reef and non-reef invertebrates and
Echinoderms and barnacles are important contributors to bioclastic limestones Echinoids are a diverse phylum with
Molluscan bioclasts are important components of tropical, and cool-temperate water limestones Bioclasts are probably the