Subvolcanic Thermodynamics - Revision history

Liam at 14:31, 11 April 2018

2018-04-11T14:31:47Z

2015-04-08T16:24:16Z

2015-03-19T12:52:14Z

2015-03-19T12:51:59Z

2015-03-13T03:33:56Z

2015-03-13T03:32:36Z

2015-03-13T03:31:17Z

2015-03-13T03:30:10Z

2015-03-13T03:29:04Z

2015-03-13T03:27:55Z

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-'''Fracture mechanics and melt in a subvolcanic magmatic breccia'''
+<h2 id="mp-itn-h2" style="margin:0.5em; width:80em; background:#cedff2; font-family:inherit; font-size:110%; font-weight:normal; border:1px solid #a3b0bf; color:#000; padding:0.2em 0.4em;">
-Sam G. Roy, Scott E. Johnson, Peter O. Koons, Zhihe Jin
+'''Abstract:''' We examine the development of a subvolcanic magmatic breccia located along the contact of
 a granitic intrusion using fractal analysis and thermal-elastic modeling. The breccia grades from clastsupported,
 angular clasts adjacent to unfractured host rock to isolated, rounded clasts supported by the
@@ Line 19: / Line 18: @@
 with high surface area to volume ratios were preferentially fractured, although this process does not appear
 to have markedly influenced the clast size distribution.
-<gallery>
+<gallery widths=400px heights=400px>
 File:1-2.png|200px|thumb|left|Frames 1-2
 File:3-4.png|200px|thumb|left|Frames 3-4
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 File:8-10.png|200px|thumb|left|Frames 8-10
 </gallery>

@@ Line 19: / Line 19: @@
 with high surface area to volume ratios were preferentially fractured, although this process does not appear
 to have markedly influenced the clast size distribution.
 <gallery>

← Older revision		Revision as of 12:52, 19 March 2015
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−	Fracture mechanics and melt in a subvolcanic magmatic breccia	+	'''Fracture mechanics and melt in a subvolcanic magmatic breccia'''

	Sam G. Roy, Scott E. Johnson, Peter O. Koons, Zhihe Jin		Sam G. Roy, Scott E. Johnson, Peter O. Koons, Zhihe Jin

← Older revision		Revision as of 12:51, 19 March 2015
Line 1:		Line 1:
		+	Fracture mechanics and melt in a subvolcanic magmatic breccia
		+
		+	Sam G. Roy, Scott E. Johnson, Peter O. Koons, Zhihe Jin
		+
	We examine the development of a subvolcanic magmatic breccia located along the contact of		We examine the development of a subvolcanic magmatic breccia located along the contact of
	a granitic intrusion using fractal analysis and thermal-elastic modeling. The breccia grades from clastsupported,		a granitic intrusion using fractal analysis and thermal-elastic modeling. The breccia grades from clastsupported,

@@ Line 1: / Line 1: @@
-This paper examines the development of a subvolcanic magmatic breccia located along the contact of
+We examine the development of a subvolcanic magmatic breccia located along the contact of
 a granitic intrusion using fractal analysis and thermal-elastic modeling. The breccia grades from clastsupported,
 angular clasts adjacent to unfractured host rock to isolated, rounded clasts supported by the

@@ Line 22: / Line 22: @@
 File:6-7.png|200px|thumb|left|Frames 6-7
 File:7b.png|200px|thumb|left|Frame 7b
 </gallery>

@@ Line 21: / Line 21: @@
 File:5.png|200px|thumb|left|Frame 5
 File:6-7.png|200px|thumb|left|Frames 6-7
 </gallery>
 [[File:Example.jpg]]