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'''Seismotectonics''' is the study of the relationship between the [[earthquakes]], active [[tectonics]] and individual [[Fault (geology)|faults]] of a region. It seeks to understand which faults are responsible for seismic activity in an area by analysing a combination of regional tectonics, recent instrumentally recorded events, accounts of historical earthquakes and [[Geomorphology|geomorphological]] evidence. This information can then be used to quantify the [[seismic hazard]] of an area.<ref name="Slejko_2012">{{Cite book |title=Recent Evolution and Seismicity of the Mediterranean Region |date=2012 |publisher=Springer |isbn=9789401120166 |editor-last=E. Boschi |editor-first=E. |chapter=A review of the Eastern Alps – Northern Dinarides Seismotectonics |editor-last2=Mantovani |editor-first2=E. |editor-last3=Morelli |editor-first3=A. |chapter-url=https://books.google.com/books?id=gbbvCAAAQBAJ&dq=seismotectonics+definition&pg=PA251}}</ref>

==Methodology==
A seismotectonic analysis of an area often involves the integration of disparate datasets.

===Regional tectonics===
An understanding of the regional tectonics of an area is likely to be derived from published [[geological map]]s, research publications on the [[structural geology|geological structure]] and [[seismic reflection]] profiles, where available, augmented by other [[geophysics|geophysical]] data.

In order to understand the seismic hazard of an area it is necessary not only to know where potentially active faults are, but also the orientation of the [[stress field]]. This is normally derived from a combination of earthquake data, borehole breakout analysis, direct stress measurement and the analysis of geologically young fault networks. The World Stress Map Project provides a useful online compilation of such data.<ref>[http://www.world-stress-map.org Website for the World Stress Map Project]</ref>

===Earthquakes===
====Instrumentally recorded events====
Since the early 20th century, sufficient information has been available from [[seismometers]] to allow the location, depth and magnitude of earthquakes to be calculated. In terms of identifying the fault responsible for an earthquake where there is no clear surface trace, recording the locations of [[aftershocks]] generally gives a strong indication of the strike of the fault.

In the last 30 years, it has been possible to routinely calculate [[focal mechanism]]s from teleseismic data. Catalogues of events with calculated focal mechanisms are now available online, such as the searchable catalogue from the [[National Earthquake Information Center|NEIC]].<ref>[https://web.archive.org/web/20070513001010/http://neic.usgs.gov/neis/sopar/ NEIC Moment Tensor and Broadband Source Parameter Search ]</ref> As focal mechanisms give two potential active fault plane orientations, other evidence is required to interpret the origin of an individual event. Although only available for a restricted time period, in areas of moderate to intense seismicity there is probably sufficient data to characterise the type of seismicity in an area, if not all the active structures.

====Historical records====
Attempts to understand the seismicity of an area require information from earthquakes before the era of instrumental recording.<ref>{{cite book|url=http://assets.cambridge.org/97805210/21876/frontmatter/9780521021876_frontmatter.pdf|last=Ambraseys|first=Nicolas|authorlink=Nicholas Ambraseys|author2=Melville, C.P. |year=1982|title=A History of Persian Earthquakes|publisher=Cambridge University Press|isbn=9780521021876}}</ref>{{rp|viii}} This requires a careful assessment of historical data in terms of their reliability. In most cases, all that can be derived is an estimate of the location and magnitude of the event. However, such data is needed to fill the gaps in the instrumental record, particularly in areas with either relatively low seismicity or where the repeat periods for major earthquakes is more than a hundred years.<ref>[http://faust.ingv.it/reports/1998-01-15/paola.htm Historical data on earthquakes and active faulting. The contribution of IRRS and IC to EC project FAUST (Contract ENV4-CT97-0428) ]</ref>

===Field investigations===
Information on the timing and magnitude of seismic events that occurred before instrumental recording can be obtained from excavations across faults that are thought to be seismically active and by studying recent sedimentary sequences for evidence of seismic activity such as [[seismite]]s<ref name="Migowski">{{cite journal|last=Migowski|first=C. |author2=Agnon A. |author3=Bookman R. |author4=Negendank J.F.W. |author5=Stein M|year=2004|title=Recurrence pattern of Holocene earthquakes along the Dead Sea transform revealed by varve-counting and radiocarbon dating of lacustrine sediments|journal=Earth and Planetary Science Letters|volume=222|issue=1 |pages=301–314|url=http://marsci.haifa.ac.il/margeo/bookmanLINK%203.PDF|accessdate=2009-12-29|bibcode = 2004E&PSL.222..301M |doi = 10.1016/j.epsl.2004.02.015 }}</ref> or [[tsunami deposit]]s.<ref name="Luque">{{cite journal|last=Luque|first=L. |author2=Lario J. |author3=Zazo C. |author4=Goy J.L. |author5=Dabrio C.J. |author6=Silva P.G.|year=2001|title=Tsunami deposits as paleoseismic indicators: examples from the Spanish coast|journal=Acta Geológica Hispánica|volume=36|issue=3–4|pages=197–211|url=http://www.raco.cat/index.php/ActaGeologica/article/viewFile/75644/107101|accessdate=2009-12-29}}</ref>

===Geomorphology===
Seismically [[active fault]]s and related fault generated [[Fold (geology)|folds]] have a direct effect on the geomorphology of a region. This may allow the direct identification of active structures not previously known. In some cases such observations can be used quantitatively to constrain the repeat period of major earthquakes, such as the [[raised beach]]es of [[Turakirae Head]] recording the history of coseismic uplift of the [[Rimutaka Range]] due to displacement on the [[Wairarapa Fault]] in [[North Island]], [[New Zealand]].<ref>[http://www.royalsociety.org.nz/Site/publish/Journals/nzjgg/2006/029.aspx McSaveney, M.J., Graham, I.J., Begg, J.G., Beu, A.G., Hull, A.G., Kyeong, K. & Zondervan, A. 2006. Late Holocene uplift of beach ridges at Turakirae Head, south Wellington coast, New Zealand. New Zealand Journal of Geology and Geophysics abstracts, 49, 337–358].</ref>

==See also==
*[[Seismology]]
*[[Plate tectonics]]

==References==
{{reflist}}

==External links==
*[http://www.geophysik.uni-muenchen.de/~igel/Lectures/Sedi/sedi_tectonics.ppt Presentation on Seismotectonics from Department of Geophysics, University of Munich]

{{Authority control}}

[[Category:Seismology]]
[[Category:Tectonics]]
[[Category:Structural geology]]

Seismotectonics - Revision history

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