Abstracts - faqs.org

Abstracts

Earth sciences

Search abstracts:
Abstracts » Earth sciences

Progressive hybridisation between Late Devonian mafic-intermediate and felsic magmas in the Meguma Zone of Nova Scotia, Canada

Article Abstract:

Three synplutonic mafic-intermediate intrusions have been found in two Late Devonian felsic plutons in the Meguma Zone of Nova Scotia, Canada. These intrusions post progressive phases of in situ hybridization. A spessartite dyke in the Port Mouton Pluton could have quickly cooled and crystallized after intrusion, while a pillowed kersantite probably contained residual magma. A diorite sheet may have acquired xenocrysts from residual magma.

Author: Tate, Marcus C., Clarke, D. Barrie, Heaman, Larry M.
Publisher: Springer
Publication Name: Contributions to Mineralogy and Petrology
Subject: Earth sciences
ISSN: 0010-7999
Year: 1997
Natural resources, Nova Scotia, Rocks, Igneous, Igneous rocks, Intrusions (Geology)

User Contributions:

Comment about this article or add new information about this topic:

CAPTCHA


Mafic magma batches at Vesuvius: a glass inclusion approach to the modalities of feeding stratovolcanoes

Article Abstract:

A study identifies the primary K-tephritic H2O-Cl-P-F-rich melts included in the olivine of 1906 lapilli as an example of primary magmas feeding Vesuvius during its recent activity. Glass inclusions in diopside and some olivine vary from K-basalt to K-tephrite with homogenization temperature of 1130-1170 degrees centigrade. The primary and near-primary Vesuvius magmas as indicated by melt inclusions are discussed.

Author: Santacroce, R., Marianelli, P., Metrich, N., Sbrana, A.
Publisher: Springer
Publication Name: Contributions to Mineralogy and Petrology
Subject: Earth sciences
ISSN: 0010-7999
Year: 1995
Olivine

User Contributions:

Comment about this article or add new information about this topic:

CAPTCHA


May 5, 1998, debris flows in circum-Vesuvian areas (southern Italy): insights for hazard assessment

Article Abstract:

Data from the May 5, 1998 debris flow from the alluvial-fan deposits east of the Vesuvius volcano has been used to develop a model to evaluate the hazard potential of similar flows for the nearby Clanio Valley. Air-fall deposits have the potential for hazards that remain decades or centuries after a volcanic eruption.

Author: Pareschi, M.T., Favalli, M., Giannini, F., Sulpizio, R., Zanchetta, G., Santacroce, R.
Publisher: Geological Society of America, Inc.
Publication Name: Geology
Subject: Earth sciences
ISSN: 0091-7613
Year: 2000
Italy, Research, Volcanoes, Hazardous geographic environments

User Contributions:

Comment about this article or add new information about this topic:

CAPTCHA


Subjects list: Analysis, Natural history, Vesuvius
Similar abstracts:
  • Abstracts: Robust strategies for abating climate change. Modeling climate change in the absence of climate change data
  • Abstracts: The relationship between concealed ovulation and mating systems in anthropoid primates: a phylogenetic analysis
  • Abstracts: Carbonate-periplatform sedimentation by density flows: a mechanism for rapid off-bank and vertical transport of shallow-water fines: comment and reply
  • Abstracts: Implications of a Bengal Fan-type deposit in the Paleozoic Lachlan fold belt of southeastern Australia. Slow late Paleozoic exhumation in the Presidential Range of New Hampshire as determined by the 40Ar/39Ar relief method: comment and reply
  • Abstracts: Distribution and tectonic setting of Ordovician K-bentonites in the United Kingdom
This website is not affiliated with document authors or copyright owners. This page is provided for informational purposes only. Unintentional errors are possible.
Some parts © 2025 Advameg, Inc.