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	<title>Neotectonics - Revision history</title>
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	<updated>2026-07-02T03:40:59Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
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		<id>http://debianws.lexgopc.com/wiki143/index.php?title=Neotectonics&amp;diff=5520663&amp;oldid=prev</id>
		<title>imported&gt;Onel5969: Disambiguating links to Tertiary (link changed to Tertiary period) using DisamAssist.</title>
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		<updated>2025-06-08T11:10:36Z</updated>

		<summary type="html">&lt;p&gt;Disambiguating links to &lt;a href=&quot;/wiki143/index.php?title=Tertiary&quot; title=&quot;Tertiary&quot;&gt;Tertiary&lt;/a&gt; (link changed to &lt;a href=&quot;/wiki143/index.php?title=Tertiary_period&quot; title=&quot;Tertiary period&quot;&gt;Tertiary period&lt;/a&gt;) using &lt;a href=&quot;/wiki143/index.php?title=User:Qwertyytrewqqwerty/DisamAssist&amp;amp;action=edit&amp;amp;redlink=1&quot; class=&quot;new&quot; title=&quot;User:Qwertyytrewqqwerty/DisamAssist (page does not exist)&quot;&gt;DisamAssist&lt;/a&gt;.&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;&amp;#039;&amp;#039;&amp;#039;Neotectonics&amp;#039;&amp;#039;&amp;#039;, a subdiscipline of [[tectonics]], is the study of the motions and deformations of [[Earth&amp;#039;s crust]] ([[geology|geological]] and [[geomorphology|geomorphological]] processes) that are current or recent in [[Geologic time scale|geologic time]].&amp;lt;ref&amp;gt;&amp;quot;Encyclopedia of Coastal Science&amp;quot; (2005), Springer, {{ISBN|978-1-4020-1903-6}}, Chapter 1: &amp;quot;Tectonics and Neotectonics&amp;quot; {{doi|10.1007/1-4020-3880-1}} &amp;lt;/ref&amp;gt; The term may also refer to the motions/deformations in question themselves. Geologists refer to the corresponding time-frame as the &amp;#039;&amp;#039;&amp;#039;neotectonic period&amp;#039;&amp;#039;&amp;#039;, and to the preceding time as the &amp;#039;&amp;#039;&amp;#039;palaeotectonic period&amp;#039;&amp;#039;&amp;#039;. &lt;br /&gt;
&lt;br /&gt;
[[Vladimir Obruchev]] coined the term &amp;#039;&amp;#039;neotectonics&amp;#039;&amp;#039; in his 1948 article,&amp;lt;ref&amp;gt;V.A. Obruchev (1948). &amp;quot;Osnovnye cherty kinetiki i plastiki neotektonik&amp;quot;. &amp;#039;&amp;#039;Izv. Akad. Nauk, Ser. Geol.&amp;#039;&amp;#039;, 5: 13–24&amp;lt;/ref&amp;gt; defining the field as &amp;quot;recent tectonic movements occurred in the upper part of [[Tertiary period|Tertiary]] ([[Neogene]]) and in the [[Quaternary]], which played an essential role in the origin of the contemporary topography&amp;quot;. Since then geologists have disagreed as to how far back to date &amp;quot;geologically recent&amp;quot; time, with the common meaning being that neotectonics is the youngest, not yet finished stage in Earth tectonics. Some authors consider neotectonics to be basically synonymous with &amp;quot;active tectonics&amp;quot;, while others date the start of the neotectonic period from the middle [[Miocene]]. A general agreement has started to emerge that the actual time-frame may be individual for each geological environment and it must be set back in time sufficiently far to fully understand the current tectonic activity.&amp;lt;ref name=koster&amp;gt;Eduard A. Koster (2005) &amp;quot;The Physical Geography of Western Europe&amp;quot;, {{ISBN|0-19-927775-3}}, [https://books.google.com/books?id=9W7ofyqW5moC&amp;amp;dq=%22neotectonics+is%22&amp;amp;pg=PA25 Ch. 2: Neotectonics]&amp;lt;/ref&amp;gt; &lt;br /&gt;
&lt;br /&gt;
In 1989 [[Spyros B. Pavlides]] suggested the definition:&lt;br /&gt;
 &lt;br /&gt;
&amp;lt;blockquote&amp;gt;&amp;quot;Neotectonics is the study of young tectonic events which have occurred or are still occurring in a given region after its [[orogeny]] or after its last significant [[tectonic set-up]] [...] The tectonic events are recent enough to permit a detailed analysis by differentiated and specific methods, while their results are directly compatible with seismological observations.&amp;quot;&amp;lt;ref&amp;gt; {{cite journal | last1 = Pavlides | first1 = Spyros B. | year = 1989 | title = Looking for a definition of neotectonics | journal = Terra Nova | volume = 1 | issue = 3| pages = 233–235 | doi = 10.1111/j.1365-3121.1989.tb00362.x }}&amp;lt;/ref&amp;gt;&amp;lt;/blockquote&amp;gt;&lt;br /&gt;
&lt;br /&gt;
Many{{howmany|date=July 2013}} researchers have accepted this approach.&amp;lt;ref name=koster/&amp;gt;&lt;br /&gt;
&lt;br /&gt;
The Center for Neotectonic Studies at the [[University of Nevada, Reno]]&amp;lt;ref name=&amp;quot;NeotectonicCenterUNR&amp;quot;&amp;gt;{{cite web |url= http://neotectonics.seismo.unr.edu/CNSHome.html |title= Center for Neotectonic Studies |author= [[University of Nevada, Reno]] }}&amp;lt;/ref&amp;gt; defines neotectonics as &lt;br /&gt;
&lt;br /&gt;
&amp;lt;blockquote&amp;gt;“the study of geologically recent motions of the [[Crust (geology)|Earth&amp;#039;s crust]], particularly those produced by [[earthquake]]s, with the goals of understanding the [[Geophysics|physics]] of [[earthquake]] recurrence, the growth of [[mountain]]s, and the [[Seismology|seismic]] hazard embodied in these processes.”&amp;lt;/blockquote&amp;gt;&lt;br /&gt;
&lt;br /&gt;
One source of different interpretations for a region stems from the fact that changes in different [[tectonic plate]]s of the region may occur at different times, giving rise to the notion of the &amp;quot;transitional time&amp;quot;, during which both palaeotectonic and neotectonic features coexist. For example, for central/northern Europe, the transitional period stretches from the middle early [[Miocene]] to the Miocene-[[Pliocene]] boundary.&amp;lt;ref&amp;gt;A. Becker, &amp;quot; An attempt to define a &amp;quot;neotectonic period&amp;quot; for central and northern Europe&amp;quot;, International Journal of Earth Sciences, Volume 82, Number 1, 1993 {{doi|10.1007/BF00563271}}&amp;lt;/ref&amp;gt;&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
* [[Seismic hazard]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&amp;lt;references/&amp;gt;&lt;br /&gt;
&lt;br /&gt;
==Further reading==&lt;br /&gt;
* P. L. Hancock and G. D. Williams,  &amp;quot;Neotectonics&amp;quot;, &amp;#039;&amp;#039;Journal of the Geological Society&amp;#039;&amp;#039;; March 1986; v. 143; no. 2; p. 325-326; {{doi|10.1144/gsjgs.143.2.0323}} (&amp;lt;!--this webpage has this strange doi code, which appears corrupted  --&amp;gt;[http://jgs.geoscienceworld.org/cgi/content/abstract/143/2/325 article abstract])&lt;br /&gt;
&lt;br /&gt;
[[Category:Tectonics]]&lt;/div&gt;</summary>
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