The link between volcanism and tectonics in the southern volcanic zone of the Chilean Andes: A review
J Cembrano, L Lara - Tectonophysics, 2009 - Elsevier
The nature of the interplay between tectonics and volcanism is a major question in
continental margin tectonics. The Southern Andes volcanic zone (SVZ), located at the …
continental margin tectonics. The Southern Andes volcanic zone (SVZ), located at the …
The tectonic framework of the Sumatran subduction zone
R McCaffrey - Annual Review of Earth and Planetary Sciences, 2009 - annualreviews.org
The great Aceh-Andaman earthquake of December 26, 2004 and its tragic consequences
brought the Sumatran region and its active tectonics into the world's focus. The plate tectonic …
brought the Sumatran region and its active tectonics into the world's focus. The plate tectonic …
Tectono-magmatic precursors for porphyry Cu-(Mo-Au) deposit formation
JP Richards - Economic geology, 2003 - pubs.geoscienceworld.org
Abstract Porphyry Cu-(Mo-Au) deposits are relatively rare but reproducible products of
subduction-related magmatism. No unique processes appear to be required for their …
subduction-related magmatism. No unique processes appear to be required for their …
Neotectonics of the Sumatran fault, Indonesia
K Sieh, D Natawidjaja - Journal of Geophysical Research: Solid …, 2000 - Wiley Online Library
The 1900‐km‐long, trench‐parallel Sumatran fault accommodates a significant amount of
the right‐lateral component of oblique convergence between the Eurasian and …
the right‐lateral component of oblique convergence between the Eurasian and …
Understanding caldera structure and development: An overview of analogue models compared to natural calderas
V Acocella - Earth-Science Reviews, 2007 - Elsevier
Understanding the structure and development of calderas is crucial for predicting their
behaviour during periods of unrest and to plan geothermal and ore exploitation. Geological …
behaviour during periods of unrest and to plan geothermal and ore exploitation. Geological …
Compressional-and transpressional-stress pattern for Pliocene and Quaternary brittle deformation in fore arc and intra-arc zones (Andes of Central and Southern …
A Lavenu, J Cembrano - Journal of Structural Geology, 1999 - Elsevier
Kinematic analysis of fault slip data for stress determination was carried out on Late Miocene
to Quaternary rocks from the fore arc and intra-arc regions of the Chilean Andes, between …
to Quaternary rocks from the fore arc and intra-arc regions of the Chilean Andes, between …
Geochemistry and tectonics of the Chilean Southern Andes basaltic Quaternary volcanism (37-46 S)
L Lopez-Escobar, J Cembrano, H Moreno - Andean geology, 1995 - andeangeology.cl
Between latitudes 37 and 46 S of the Andes, the Nazca-South America Plate convergence is
currently slightly oblique, Postglacial volcanism has been continuous and intense, being …
currently slightly oblique, Postglacial volcanism has been continuous and intense, being …
Structure of volcano plumbing systems: A review of multi-parametric effects
A Tibaldi - Journal of Volcanology and Geothermal Research, 2015 - Elsevier
Magma is transported and stored in the crust mostly through networks of planar structures
(intrusive sheets), ranging from vertical dykes to inclined sheets and horizontal sills, and …
(intrusive sheets), ranging from vertical dykes to inclined sheets and horizontal sills, and …
The Toba caldera complex
CA Chesner - Quaternary International, 2012 - Elsevier
The Toba Caldera in Indonesia is one of the most remarkable volcanic features formed
during Quaternary geologic time. Its rich history of research for over a century has yielded …
during Quaternary geologic time. Its rich history of research for over a century has yielded …
Transpressional kinematics and magmatic arcs
Most continental magmatic arcs occur in obliquely convergent settings and display strike-slip
movement within, or adjacent to, the magmatic arc, and contractional structures in the …
movement within, or adjacent to, the magmatic arc, and contractional structures in the …