Earth-prints repository, logo   DSpace

About DSpace Software
|earth-prints home page | roma library | bologna library | catania library | milano library | napoli library | palermo library
Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/4999

Authors: Calderoni, G.*
Di Giovambattista, R.*
Burrato, P.*
Ventura, G.*
Title: A seismic sequence from Northern Apennines (Italy) provides new insight on the role of fluids in the active tectonics of accretionary wedges
Title of journal: Earth and Planetary Science Letters
Series/Report no.: 1-2/281 (2008)
Publisher: Elsevier
Issue Date: Apr-2009
DOI: 10.1016/j.epsl.2009.02.015
URL: http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6V61-4VRNNRY-3&_user=5381242&_coverDate=04%2F30%2F2009&_rdoc=11&_fmt=high&_orig=browse&_srch=doc-info(%23toc%235801%232009%23997189998%231016088%23FLA%23display%23Volume)&_cdi=5801&_sort=d&_docanchor=&_ct=13&_acct=C000067082&_version=1&_urlVersion=0&_userid=5381242&md5=70870b42d730bb7f3463469a1c4a60d0
Keywords: seismicity
fluids
accretionary wedge
thrust
geodynamics
Northern Apennines
Abstract: We analyze a seismic sequence which occurred in 2000 along the Northern Apennines accretionary wedge (Italy). The sequence developed within the Cretaceous–Triassic limestones of the tectonic wedge, where methane-rich and oil reservoirs are stored. Ruptures mainly developed on WNW–ESE striking thrusts. The compressive stress field is consistent with that acting at regional scale in Northern Apennines. Seismic parameters indicate that fluids are involved in the seismogenic process. The amplitudes of the P and S phases and data from some stations evidence a P to S conversion within Vp/Vs=2.1 layer. The attenuation properties of crust show a higher attenuation zone located west of the epicentral cloud. Eight hundred aftershocks delineate a sub-vertical cloud of events between 7 and 14 km depth. The space–time evolution of the aftershocks is consistent with a diffusive spreading (diffusivity=1.9 m2/s) along vertically superimposed thrusts. Diffusion also controls the time evolution of the sequence. Fluid pressure is estimated to be roughly equal to the vertical, lithostatic stress. The overpressure within reservoirs develops by tectonic compaction processes. The fluids upraise along sub-vertical fractures related to the shortening of the wedge. The 2000 sequence occurred in an area that separates a thermal and deeper petroleum system from a shallower biogenic system. The divider of these systems controls the attenuation properties of the crust. The fluid–rock interaction at seismogenetic depth is related to hydrothermal processes more than to compaction. In accretionary wedges, seismicity activating superimposed thrusts may drive methane and oil upraising from the upper crust.
Appears in Collections:04.06.09. Waves and wave analysis
04.06.03. Earthquake source and dynamics
04.04.01. Earthquake geology and paleoseismology
04.06.01. Earthquake faults: properties and evolution
Papers Published / Papers in press

Files in This Item:

File Description SizeFormatVisibility
Calderoni_etal_revised.pdfCorrected manuscript5.81 MBAdobe PDFView/Open
Calderoni_etal_2009_EPSL.pdfPrinted paper1.84 MBAdobe PDFView/Open

This item is licensed under a Creative Commons License
Creative Commons


Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.


Share this record
Del.icio.us

Citeulike

Connotea

Facebook

Stumble it!

reddit


 

Valid XHTML 1.0! ICT Support, development & maintenance are provided by CINECA. Powered on DSpace Software. CINECA