Geometric Scaling of Tabular Igneous Intrusions: Implications for Emplacement and Growth

Alexander Ramsay Cruden, Kenneth J.W. McCaffrey, Andrew Bunger

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Abstract

The horizontal (L) and vertical (T) dimensions of broadly tabular, sub-horizontal intrusions of mafic to felsic composition emplaced into shallow to mid-crustal levels of continental crust reveal two well-defined and continuous curves in log L vs. log T space. The data set spans six and five orders of magnitude in L (1 m to 1000 km) and T (10 cm to 10 km), respectively. Small tabular sheets and sills (mafic and felsic) define a straight line with a slope * 0.5 at all horizontal length scales, similar to the known geometric scaling of mafic dikes, indicating that the L/T ratio of these intrusions to increases with increasing L (horizontal lengthening dominates over vertical thickening). Laccoliths, plutons, layered mafic intrusions and batholiths define an open, continuous S-shaped curve that bifurcates from the tabular sheets and sills curve at L * 500 m towards higher T values. For L * 0.5 to 10 km the slope of this curve is * 1.5, corresponding to laccoliths that are characterized by a decrease in L/T ratio with increasing L (vertical thickening dominates over horizontal lengthening). Between L * 10 and 100 km the slope has a mean value * 0.8, indicating that plutons and layered mafic intrusions have a tendency for horizontal lengthening over vertical thickening as L increases. Batholiths and very large layered mafic intrusions with L > 100 km lie on a slope * 0 with a threshold thickness * 10 km. The continuous nature of the dimensional data over such a wide range of length scales reflects a spectrum of igneous emplacement processes repeated in space and time. We discuss how thresholds and transitions in this spectrum, defined by bifurcations between the curves (e.g., between sill and laccolith emplacement) and changes in slope, largely reflect depth- and time-dependent changes in emplacement mechanisms rather than factors such as magma viscosity, composition and temperature.
Original languageEnglish
Title of host publicationPhysical Geology of Shallow Magmatic Systems
Subtitle of host publicationDykes, Sills and Laccoliths
EditorsChristoph Breitkreuz, Sergio Rocchi
Place of PublicationSwitzerland
PublisherSpringer
Chapter2
Pages11-38
Number of pages27
Edition1
ISBN (Electronic)2364-3285
ISBN (Print)2364-3277
Publication statusPublished - 2018

Publication series

NameAdvances in Volcanology: An Official Book Series of the International Association of Volcanology and Chemistry of the Earth’s Interior
PublisherSpringer
ISSN (Print)2364-3277
ISSN (Electronic)2364-3285

Cite this

Cruden, A. R., McCaffrey, K. J. W., & Bunger, A. (2018). Geometric Scaling of Tabular Igneous Intrusions: Implications for Emplacement and Growth. In C. Breitkreuz, & S. Rocchi (Eds.), Physical Geology of Shallow Magmatic Systems: Dykes, Sills and Laccoliths (1 ed., pp. 11-38). (Advances in Volcanology: An Official Book Series of the International Association of Volcanology and Chemistry of the Earth’s Interior). Springer.