Crustal extension from exposed sheet intrusions: review and method proposal

Authors
Citation
Lb. Marinoni, Crustal extension from exposed sheet intrusions: review and method proposal, J VOLCANOL, 107(1-3), 2001, pp. 27-46
Citations number
65
Language
INGLESE
art.tipo
Review
Categorie Soggetti
Earth Sciences
Journal title
JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH
ISSN journal
0377-0273 → ACNP
Volume
107
Issue
1-3
Year of publication
2001
Pages
27 - 46
Database
ISI
SICI code
0377-0273(200106)107:1-3<27:CEFESI>2.0.ZU;2-U
Abstract
Sheet intrusions are probably the most widespread magmatic features on Eart h. They create a space for themselves by dilating the host rock. The expose d sheet intrusions allow an estimate of a minimum value of the extension to which the crustal layers and the volcanic edifices are subject. The correc t evaluation of the contribution of sheet intrusions to the crustal extensi on is of great importance in various geologic settings. The current methods used to evaluate the extension due to exposed sheet intrusions are reviewe d in this paper. The effect of the dip of sheet intrusions on the evaluatio n of horizontal crustal extension is analysed. If the dip effect is neglect ed and the intrusions are (sub)vertical, the error due to the dip effect in the extension evaluation is small; if the intrusions are shallow dipping, the error may be great and varies as a function of the dyke dip. For dykes with dip range 45-65 degrees, the error due to neglecting the dip effect is similar to 30 to similar to 15%. Increasing discrepancies of more than 25% are produced on the computed dilation when the intrusions progressively di p less than 50 degrees. A simple method, based on structural field measurem ents of exposed sheet intrusions and on trigonometric considerations, is pr esented as an improvement of pre-existing methods to estimate the horizonta l component of the crustal extension. Using this method, field data of 1154 dykes from different geodynamic contexts are analysed. The horizontal comp onent of extension is computed using dyke data from the Tertiary massifs of Lanzarote and Tenerife, and from the active stratovolcanoes of Monte Somma -Vesuvius and Etna. Since the analysed dykes are steeply dipping, the cumul ative difference between the extension computed neglecting and taking into account the dip effect remains less than 10% for ail the data sets. The per centage difference is nearly constant and cumulatively higher for Monte Som ma, where the mean dip of the intrusions is smaller. In Lanzarote, 237 dyke s emplaced between similar to 15.5 and similar to3.7 Ma give a peak extensi on of 276 m in direction N135 degrees, and a time-averaged minimum extensio n rate of 1.9 x 10(-2) to 2.3 X 10(-2) mm a(-1). In Tenerife, an extension of 562 m is computed in the direction N65 degrees from 563 dykes emplaced f rom similar to7.4 to similar to3.3 Ma. The time-averaged minimum rate of ex tension for the Tertiary massifs of Tenerife ranges from 0.14 to 0.25 mm a( -1). The peak extension computed for Monte Somma is 81.7 m in the direction N90 degrees, based on 96 exposed sheets. Very likely, most of Monte Somma sheets intruded within similar to 12 ka, giving a time-averaged minimum ext ension rate of similar to7 mm a(-1). From 184 exposed dykes of Etna, a mini mum extension rate of 6.2 mm a(-1) is computed (peak extension is 212 m in direction N35 degrees). The poor resolution of age constraints may affect d eeply the reliability of the extension rates. However. from the examples pr esented it appears that the extension rates of pre-erosional successions fr om intraplate volcanic islands can be smaller than those of active stratovo lcanoes. This may suggest a more active dynamics in the stratovolcanoes. (C ) 2001 Elsevier Science B.V. All rights reserved.