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Vertically extensive and unstable magmatic systems: a unified view of igneous processes
BACKGROUND For more than 100 years, the melt-dominated magma chamber has been
central to conceptual models of volcanism and igneous processes. Over the past few …
central to conceptual models of volcanism and igneous processes. Over the past few …
[HTML][HTML] Layered intrusions: Fundamentals, novel observations and concepts, and controversial issues
Layered intrusions are fossilized natural laboratories that historically have constrained many
fundamental principles of igneous petrology. Layered intrusions are typically stratiform …
fundamental principles of igneous petrology. Layered intrusions are typically stratiform …
Architecture and dynamics of magma reservoirs
This introductory article provides a synopsis of our current understanding of the form and
dynamics of magma reservoirs in the crust. This knowledge is based on a range of …
dynamics of magma reservoirs in the crust. This knowledge is based on a range of …
Magmatic volatiles (H, C, N, F, S, Cl) in the lunar mantle, crust, and regolith: Abundances, distributions, processes, and reservoirs
Many studies exist on magmatic volatiles (H, C, N, F, S, Cl) in and on the Moon, within the
last several years, that have cast into question the post-Apollo view of lunar formation, the …
last several years, that have cast into question the post-Apollo view of lunar formation, the …
[کتاب][B] Basalts and phase diagrams
SA Morse - 1980 - Springer
Basalt is the most abundant rock on Earth. It forms the ocean ridges, slides off onto the
ocean fioor, and eventually dives back down. Basalt is the lava which pours out of Kilauea in …
ocean fioor, and eventually dives back down. Basalt is the lava which pours out of Kilauea in …
Crystallization sequence and magma chamber processes in the ferrobasaltic Sept Iles layered intrusion, Canada
Abstract The Sept Iles layered intrusion (Quebec, Canada; 564 Ma) is a large plutonic body
with a diameter of 80 km and a thickness of 6 km made up from its base to top of a layered …
with a diameter of 80 km and a thickness of 6 km made up from its base to top of a layered …
Assessing the role of compaction in the formation of adcumulates: a microstructural perspective
The formation of adcumulates necessitates the continued growth of primocrysts down to low
porosities. Gravitationally driven viscous compaction at the base of a crystal mushy layer on …
porosities. Gravitationally driven viscous compaction at the base of a crystal mushy layer on …
Silicate liquid immiscibility within the crystal mush: late-stage magmatic microstructures in the Skaergaard intrusion, East Greenland
Late-stage microstructures developed during the last stages of solidification of the
Skaergaard intrusion comprise a wide array of reactive and non-reactive intergrowths …
Skaergaard intrusion comprise a wide array of reactive and non-reactive intergrowths …
Differentiation and compaction in the Skaergaard intrusion
Igneous differentiation processes are constrained from bulk compositions, densities and
mineral modes of 116 cumulate gabbro samples in a new reference profile through the …
mineral modes of 116 cumulate gabbro samples in a new reference profile through the …
Crystallization of the Skaergaard intrusion from an emulsion of immiscible iron-and silica-rich liquids: evidence from melt inclusions in plagioclase
The presence of Fe-and Si-rich liquids found as melt inclusions in apatite and olivine in the
Upper Zone of the Skaergaard intrusion, East Greenland, demonstrates the occurrence of …
Upper Zone of the Skaergaard intrusion, East Greenland, demonstrates the occurrence of …