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		<id>https://en.formulasearchengine.com/index.php?title=List_of_unsolved_problems_in_physics&amp;diff=2724</id>
		<title>List of unsolved problems in physics</title>
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		<summary type="html">&lt;p&gt;155.185.21.72: /* Quantum mechanics */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;{{Unreferenced|date=December 2009}}&lt;br /&gt;
&#039;&#039;&#039;Thermal history modelling&#039;&#039;&#039; is an exercise undertaken during [[basin modelling]] to evaluate the temperature history of stratigraphic layers in a [[sedimentary basin]].&lt;br /&gt;
&lt;br /&gt;
The thermal history of a basin is usually calibrated using thermal indicator data, including [[vitrinite]] reflectance and [[fission track]]s in the [[mineral]]s [[apatite]] and [[zircon]].&lt;br /&gt;
&lt;br /&gt;
The temperatures undergone by rocks in a sedimentary basin are crucial when attempting to evaluate the quantity, nature and volume of [[hydrocarbon]]s ([[fossil fuel]]s) produced by [[diagenesis]] of [[kerogen]]s (a group of chemicals formed from the decay of organic matter).&lt;br /&gt;
&lt;br /&gt;
[[Jean Baptiste Joseph Fourier|Fourier&#039;s]] [[Fourier&#039;s Law|Law]] provides a simplified one-dimensional description of the variation in heat flow &#039;&#039;Q&#039;&#039; as a function of [[thermal conductivity]] &#039;&#039;k&#039;&#039; and thermal gradient &#039;&#039;dT&#039;&#039;/&#039;&#039;dz&#039;&#039;:&lt;br /&gt;
&lt;br /&gt;
:&amp;lt;math&amp;gt;Q=-k\frac{dT}{dz}&amp;lt;/math&amp;gt;&lt;br /&gt;
&lt;br /&gt;
(The minus sign indicates that heat flows in the opposite direction to increasing depth, that is, towards the Earth&#039;s surface.)&lt;br /&gt;
&lt;br /&gt;
If the assumptions used to justify this simplified approximation (i.e. steady-state [[heat conduction]], no [[convection]] or [[advection]]) are accepted, we define the simple 1-dimensional heat diffusion equation where temperature &#039;&#039;T&#039;&#039; at a depth &#039;&#039;z&#039;&#039; and time &#039;&#039;t&#039;&#039; is given by the equation:&lt;br /&gt;
&lt;br /&gt;
:&amp;lt;math&amp;gt;T_{z,t} = T_{t}^0 + Q_t \int_0^z\frac{dz&#039;}{k_{z&#039;}}&amp;lt;/math&amp;gt;&lt;br /&gt;
where &#039;&#039;T&#039;&#039;&amp;lt;sub&amp;gt;t&amp;lt;/sub&amp;gt;&amp;lt;sup&amp;gt;0&amp;lt;/sup&amp;gt; is the surface temperature history, &#039;&#039;Q&#039;&#039;&amp;lt;sub&amp;gt;&#039;&#039;t&#039;&#039;&amp;lt;/sub&amp;gt; is the [[heat flow]] history and &#039;&#039;k&#039;&#039; is thermal conductivity.  The integral thus represents the integrated thermal conductivity history of a 1-dimensional column of rock.&lt;br /&gt;
&lt;br /&gt;
Thermal history modelling attempts to describe the temperature history &#039;&#039;T&#039;&#039;&amp;lt;sub&amp;gt;z,t&amp;lt;/sub&amp;gt; and therefore requires a knowledge of the burial history of the stratigraphic layers which is obtained through the process of [[back-stripping]].&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
*[[Petroleum geology]]&lt;br /&gt;
&lt;br /&gt;
{{DEFAULTSORT:Thermal History Modelling}}&lt;br /&gt;
[[Category:Petroleum geology]]&lt;br /&gt;
[[Category:Sedimentology]]&lt;/div&gt;</summary>
		<author><name>155.185.21.72</name></author>
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