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Layered Intrusions

Part of the Springer Geology Book Series

Editors: Charlier, Bernard; Namur, Olivier; Latypov, Rais; Tegner, Christian

DOI: 10.1007/978-94-017-9652-1

ISBN: 978-94-017-9651-4

Publisher: Springer Netherlands - Springer Journals

May 19, 2015

1 - 10 of 15 Chapters

LitStream

Geochronology of Layered Intrusions

Scoates, James S.; Wall, Corey J.

Pages: 3 –74

[Layered intrusions crystallize mainly from basaltic magma to form large bodies of igneous rocks that exhibit prominent layering and they preserve stunning rock records of the processes by which magma evolves in crustal magma chambers. These intrusions contain world-class deposits of chromium,...
LitStream

Igneous Layering in Basaltic Magma Chambers

Namur, O.; Abily, Bénédicte; Boudreau, Alan E.; Blanchette, Francois; Bush, John W. M.; Ceuleneer, Georges; Charlier, B.; Donaldson, Colin H.; Duchesne, Jean-Clair; Higgins, M. D.; Morata, D.; Nielsen, Troels F. D.; O’Driscoll, B.; Pang, K. N.; Peacock, Thomas; Spandler, Carl J.; Toramaru, Atsushi; Veksler, I.V.

Pages: 75 –152

[Layering is a common feature in mafic and ultramafic layered intrusions and generally consists of a succession of layers characterized by contrasted mineral modes and/or mineral textures, including grain size and orientation and, locally, changing mineral compositions. The morphology of the...
LitStream

Quantitative Textural Analysis of Rocks in Layered Mafic Intrusions

Higgins, Michael D.

Pages: 153 –181

[Quantification of rock textures (= microstructures), in the form of crystal sizes, shapes and orientations, complements chemical and isotopic approaches to the determination of the petrogenesis of rocks in layered mafic intrusions. Textures develop initially by nucleation and kinetic growth, but...
LitStream

The Influence of Interfacial Energies on Igneous Microstructures

Holness, Marian B.; Vernon, Ron H.

Pages: 183 –228

[The thermal history of igneous rocks is encoded in their microstructures via the control by cooling rate on crystal growth. If temperatures remain close to the liquidus, with small undercoolings, growth rates are low and microstructures are strongly affected by constraints imposed by interfacial...
LitStream

Silicate Liquid Immiscibility in Layered Intrusions

Veksler, Ilya V.; Charlier, Bernard

Pages: 229 –258

[More and more evidence for the development of silicate liquid immiscibility during cooling of magmas in layered intrusions have been presented. Here, we review some theoretical principles with a focus on the separation of two silicate melts, i.e. silica-rich vs. iron-rich. We discuss the role of...
LitStream

Basal Reversals in Mafic Sills and Layered Intrusions

Latypov, Rais

Pages: 259 –293

[Fractional crystallization of ponded basaltic magma results in rocks that become increasingly more evolved in composition inwards. However, almost all mafic sills and layered intrusions show basal reversals tens to hundreds of meters thick in which minerals and rocks become compositionally more...
LitStream

The Significance of Magnetic Fabric in Layered Mafic-Ultramafic Intrusions

O’Driscoll, Brian; O’Driscoll, Brian; Ferré, Eric C.; Stevenson, Carl T. E.; Magee, Craig

Pages: 295 –329

[Anisotropy of magnetic susceptibility (AMS) has been recognised as a well-established fabric analysis tool for intrusive igneous rocks since the 1990s. The AMS technique provides directional information for magnetic foliation and magnetic lineation fabric components of the AMS ellipsoid,...
LitStream

Physical Controls of Nucleation, Growth and Migration of Vapor Bubbles in Partially Molten Cumulates

Mungall, James E.

Pages: 331 –377

[The interstitial melt in partially molten cumulate piles in layered intrusions must at some point reach saturation with a volatile phase such as water vapor or hydrosaline melt. A number of models have been proposed in which orthomagmatic fluids migrate through partially solidified cumulates and...
LitStream

Platinum-Group Element Deposits in Layered Intrusions: Recent Advances in the Understanding of the Ore Forming Processes

Godel, Bélinda

Pages: 379 –432

[The major deposits of platinum-group elements (PGE) of the Earth are associated with ultramafic and mafic igneous rocks. The bulk of current PGE production is extracted from narrow stratiform horizons referred to as reefs located in the lower to central portions of large layered intrusions and...
LitStream

The Panzhihua Intrusion, SW China

Pang, Kwan-Nang; Shellnutt, J. Gregory; Zhou, Mei-Fu

Pages: 435 –463

[The ~ 260 Ma Panzhihua intrusion is an elongate layered gabbroic intrusion with a length of ~ 19 km and a thickness of ~ 2 km in the central part of the Emeishan large igneous province, SW China. It is made up from the base to top of microgabbros (Marginal zone, MGZ), gabbros, oxide gabbros and...

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