Mafic microgranular enclaves (MMEs) trace the origin of post-collisional magmas

Paleoproterozoic Shoshonite Mafic Associations of the Irkut Block (Sharyzhalgai Uplift, Southwest Siberian Craton): U–Pb Age and Conditions of Zircon Crystallization

Syn-collisional extension and Ni-Cu sulfide-bearing mafic magma emplacement along the Irtysh Shear Zone in the Central Asian Orogenic Belt

Catastrophic craton destruction via wholesale lithosphere delamination

Pyroxenite melting at subduction zones

Quantitative record of the Neoarchean water cycle from a 2.67 Ga magmatic-hydrothermal system, Fennoscandian Shield

Europium anomalies in detrital zircons record major transitions in Earth geodynamics at 2.5 Ga and 0.9 Ga

Europium anomalies in detrital zircons record major transitions in Earth geodynamics at 2.5 Ga and 0.9 Ga

Post-subduction porphyry Cu magmas in the Sanjiang region of southwestern China formed by fractionation of lithospheric mantle–derived mafic magmas

Eocene magmatism in the Himalaya: Response to lithospheric flexure during early Indian collision?

Migration and tectonic implications of Late Jurassic mafic magmatism in South China

Transition to magma-driven rifting in the South Turkana Basin, Kenya: Part 2

Magnetite-rutile symplectite in ilmenite records magma hydration in layered intrusions

Zircon Petrochronology of the Kışladaǧ Porphyry Au Deposit (Turkey)

Generation of the Giant Porphyry Cu-Au Deposit by Repeated Recharge of Mafic Magmas at Pulang in Eastern Tibet

Transport of mafic magma through the crust and sedimentary basins: Jameson Land, East Greenland

In Situ Multiple Sulfur Isotope and S/Se Composition of Magmatic Sulfide Occurrences in the Labrador Trough, Northern Quebec

Formation of ultrapotassic magma via crustal contamination and hybridization of mafic magma: an example from the Stomanovo monzonite, Central Rhodope Massif, Bulgaria

A High-Pressure Thermal Aureole of the Bayan-Kol Gabbro–Monzodiorite Intrusion (Western Sangilen, Southeastern Tuva): Evidence for Lower-Crust Mafic Magma Chambers

Constraints on deep, CO 2 -rich degassing at arc volcanoes from solubility experiments on hydrous basaltic andesite of Pavlof Volcano, Alaska Peninsula, at 300 to 1200 MPa