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Growth of a volcanic edifice through plumbing system processes-volcanic rift zones, magmatic sheet-intrusion swarms and long-lived conduits

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Growth of a volcanic edifice through plumbing system processes-volcanic rift zones, magmatic sheet-intrusion swarms and long-lived conduits. / Burchardt, Steffi; Walter, Thomas R.; Tuffen, Hugh.
Volcanic and Igneous Plumbing Systems: Understanding Magma Transport, Storage, and Evolution in the Earth's Crust. ed. / Steffi Burchardt. Elsevier, 2018. p. 89-112.

Research output: Contribution in Book/Report/Proceedings - With ISBN/ISSN › Chapter

Harvard

Burchardt, S, Walter, TR & Tuffen, H 2018, Growth of a volcanic edifice through plumbing system processes-volcanic rift zones, magmatic sheet-intrusion swarms and long-lived conduits. in S Burchardt (ed.), Volcanic and Igneous Plumbing Systems: Understanding Magma Transport, Storage, and Evolution in the Earth's Crust. Elsevier, pp. 89-112. https://doi.org/10.1016/B978-0-12-809749-6.00004-2

APA

Burchardt, S., Walter, T. R., & Tuffen, H. (2018). Growth of a volcanic edifice through plumbing system processes-volcanic rift zones, magmatic sheet-intrusion swarms and long-lived conduits. In S. Burchardt (Ed.), Volcanic and Igneous Plumbing Systems: Understanding Magma Transport, Storage, and Evolution in the Earth's Crust (pp. 89-112). Elsevier. https://doi.org/10.1016/B978-0-12-809749-6.00004-2

Vancouver

Burchardt S, Walter TR, Tuffen H. Growth of a volcanic edifice through plumbing system processes-volcanic rift zones, magmatic sheet-intrusion swarms and long-lived conduits. In Burchardt S, editor, Volcanic and Igneous Plumbing Systems: Understanding Magma Transport, Storage, and Evolution in the Earth's Crust. Elsevier. 2018. p. 89-112 doi: 10.1016/B978-0-12-809749-6.00004-2

Author

Burchardt, Steffi ; Walter, Thomas R. ; Tuffen, Hugh. / Growth of a volcanic edifice through plumbing system processes-volcanic rift zones, magmatic sheet-intrusion swarms and long-lived conduits. Volcanic and Igneous Plumbing Systems: Understanding Magma Transport, Storage, and Evolution in the Earth's Crust. editor / Steffi Burchardt. Elsevier, 2018. pp. 89-112

Bibtex

@inbook{12f0dbf4772e480fab7113940d38141e,
title = "Growth of a volcanic edifice through plumbing system processes-volcanic rift zones, magmatic sheet-intrusion swarms and long-lived conduits",
abstract = "The shallow plumbing system of volcanoes usually comprises countless magmatic sheet intrusions that can transport magma from a magma reservoir towards the surface. These sheet intrusions have characteristic shapes with straight, steeply dipping sheets generally referred to as dykes and conical, shallow- to moderately dipping sheets called cone sheets. Magmatic sheets arrange in systematic patterns, such as elongate volcanic rift zones, concentric cone-sheet swarms and radial dyke swarms. All three types of sheets may form in the same volcano and be fed from the same magma chamber. It is the geometrical relationship between the depth and the size of the feeder, as well as viscous stresses that result from the interplay between the properties of the magma and its host rock that control whether cone sheets or dykes form. Moreover, the gravitational force exerted by the volcanic edifice and regional tectonic stresses that produce a radial or elongate rift-one arrangement of dykes. At the Earth{\textquoteright}s surface, sheet intrusions feed fissure eruptions that with time can develop into pipe-like conduits.",
keywords = "Conduit, Cone sheet, Dyke swarm, Inclined sheet, Intrusive growth, Magmatic sheet intrusions, Radial dyke, Volcanic rift zone",
author = "Steffi Burchardt and Walter, {Thomas R.} and Hugh Tuffen",
year = "2018",
month = jan,
day = "1",
doi = "10.1016/B978-0-12-809749-6.00004-2",
language = "English",
isbn = "9780128097502",
pages = "89--112",
editor = "Burchardt, {Steffi }",
booktitle = "Volcanic and Igneous Plumbing Systems",
publisher = "Elsevier",
address = "Netherlands",

}

RIS

TY - CHAP

T1 - Growth of a volcanic edifice through plumbing system processes-volcanic rift zones, magmatic sheet-intrusion swarms and long-lived conduits

AU - Burchardt, Steffi

AU - Walter, Thomas R.

AU - Tuffen, Hugh

PY - 2018/1/1

Y1 - 2018/1/1

N2 - The shallow plumbing system of volcanoes usually comprises countless magmatic sheet intrusions that can transport magma from a magma reservoir towards the surface. These sheet intrusions have characteristic shapes with straight, steeply dipping sheets generally referred to as dykes and conical, shallow- to moderately dipping sheets called cone sheets. Magmatic sheets arrange in systematic patterns, such as elongate volcanic rift zones, concentric cone-sheet swarms and radial dyke swarms. All three types of sheets may form in the same volcano and be fed from the same magma chamber. It is the geometrical relationship between the depth and the size of the feeder, as well as viscous stresses that result from the interplay between the properties of the magma and its host rock that control whether cone sheets or dykes form. Moreover, the gravitational force exerted by the volcanic edifice and regional tectonic stresses that produce a radial or elongate rift-one arrangement of dykes. At the Earth’s surface, sheet intrusions feed fissure eruptions that with time can develop into pipe-like conduits.

AB - The shallow plumbing system of volcanoes usually comprises countless magmatic sheet intrusions that can transport magma from a magma reservoir towards the surface. These sheet intrusions have characteristic shapes with straight, steeply dipping sheets generally referred to as dykes and conical, shallow- to moderately dipping sheets called cone sheets. Magmatic sheets arrange in systematic patterns, such as elongate volcanic rift zones, concentric cone-sheet swarms and radial dyke swarms. All three types of sheets may form in the same volcano and be fed from the same magma chamber. It is the geometrical relationship between the depth and the size of the feeder, as well as viscous stresses that result from the interplay between the properties of the magma and its host rock that control whether cone sheets or dykes form. Moreover, the gravitational force exerted by the volcanic edifice and regional tectonic stresses that produce a radial or elongate rift-one arrangement of dykes. At the Earth’s surface, sheet intrusions feed fissure eruptions that with time can develop into pipe-like conduits.

KW - Conduit

KW - Cone sheet

KW - Dyke swarm

KW - Inclined sheet

KW - Intrusive growth

KW - Magmatic sheet intrusions

KW - Radial dyke

KW - Volcanic rift zone

U2 - 10.1016/B978-0-12-809749-6.00004-2

DO - 10.1016/B978-0-12-809749-6.00004-2

M3 - Chapter

AN - SCOPUS:85059767534

SN - 9780128097502

SP - 89

EP - 112

BT - Volcanic and Igneous Plumbing Systems

A2 - Burchardt, Steffi

PB - Elsevier

ER -