Appinite complexes preserve evidence of mantle processes that produce voluminous
granitoid batholiths. These plutonic complexes range from ultramafic to felsic in composition …

This chapter explores the growing body of stable and radiogenic Ca isotope measurements
in high temperature terrestrial materials and covers the emerging applications for Ca isotope …

Abstract The early Ediacaran Capela pluton (ca. 630 Ma) is intruded into the
metasedimentary succession of the Sergipano Orogenic System along the oriental segment …

Although the voluminous granitoids that constitute the upper crust of the Sierra Nevada
batholith (California) have been investigated in detail, comparatively few studies focus on …

Kinetic calcium isotope effects can be used as growth-rate proxies for volcanic and
subvolcanic minerals. Here, we analyze Ca isotopic compositions in experimental and …

Appinite bodies are a suite of plutonic rocks, ranging from ultramafic to felsic in composition,
that are characterized by idiomorphic hornblende as the dominant mafic mineral in all …

The appinite suite of rocks offers a unique opportunity to reveal the properties of subarc
lithospheric mantle, indicate essential crust-mantle interactions, and ascertain critical …

We present textural and chemical analyses of minerals from a 150 m thick sequence of
submarine mid-ocean ridge basalts from the South China Sea in order to showcase the …

Magmatic superheating is a condition with relevance to natural systems as well as
experimental studies of crystallization kinetics. Magmas on Earth and other planetary bodies …

Crystallization timescales in subvolcanic systems and the consequences of interaction
between ascending magmas and gases remain largely unconstrained, as do links between …