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	<id>https://en.banglapedia.org/index.php?action=history&amp;feed=atom&amp;title=Chalcopyrite</id>
	<title>Chalcopyrite - Revision history</title>
	<link rel="self" type="application/atom+xml" href="https://en.banglapedia.org/index.php?action=history&amp;feed=atom&amp;title=Chalcopyrite"/>
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	<updated>2026-06-15T09:30:38Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
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	<entry>
		<id>https://en.banglapedia.org/index.php?title=Chalcopyrite&amp;diff=13931&amp;oldid=prev</id>
		<title>Mukbil at 11:39, 18 September 2021</title>
		<link rel="alternate" type="text/html" href="https://en.banglapedia.org/index.php?title=Chalcopyrite&amp;diff=13931&amp;oldid=prev"/>
		<updated>2021-09-18T11:39:16Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table style=&quot;background-color: #fff; color: #202122;&quot; data-mw=&quot;interface&quot;&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 11:39, 18 September 2021&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l1&quot;&gt;Line 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&#039;&#039;&#039;Chalcopyrite&#039;&#039;&#039; ore mineral of copper; crystallises in the tetragonal crystal system, but crystals are generally small with diphenoidal faces resembling the tetrahedron; usually massive with a metallic lustre and brass or golden-yellow colour; shows greenish-black streaks, uneven fracture and indistinct cleavage; hardness is 3.5-4 on Moh&#039;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;;&lt;/del&gt;s scale and specific gravity is 4.1-4.3. Chalcopyrite is also known as copper pyrite or yellow pyrite and because of its physical appearance it is also called &#039;fools&#039;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;; &lt;/del&gt;gold&#039;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;;&lt;/del&gt;. It occurs in mesothermal or hypothermic deposits. The upper part of the Rajmahal Traps has been highly weathered and there is indication of the presence of chalcopyrite and chalcocite in the rocks. However, chalcopyrite is not very stable as it has low hardness as compared to other heavy minerals and as such it is extremely rare in heavy mineral suites of various vertical sections of the Chittagong, Chittagong Hill Tracts and [[surma basin]] of Bangladesh and [[assam]] and [[tripura]] states of India. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[Sifatul Quader Chowdhury] [Chowdhury, Sifatul Quader  Professor of Geology, Dhaka University]&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&#039;&#039;&#039;Chalcopyrite&#039;&#039;&#039; &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt; &lt;/ins&gt;ore mineral of copper; crystallises in the tetragonal crystal system, but crystals are generally small with diphenoidal faces resembling the tetrahedron; usually massive with a metallic lustre and brass or golden-yellow colour; shows greenish-black streaks, uneven fracture and indistinct cleavage; hardness is 3.5-4 on Moh&#039;s scale and specific gravity is 4.1-4.3. Chalcopyrite is also known as copper pyrite or yellow pyrite and because of its physical appearance it is also called &#039;fools&#039; gold&#039;. It occurs in mesothermal or hypothermic deposits. The upper part of the Rajmahal Traps has been highly weathered and there is indication of the presence of chalcopyrite and chalcocite in the rocks. However, chalcopyrite is not very stable as it has low hardness as compared to other heavy minerals and as such it is extremely rare in heavy mineral suites of various vertical sections of the Chittagong, Chittagong Hill Tracts and [[&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Surma Basin|&lt;/ins&gt;surma basin]] of Bangladesh and [[assam]] and [[tripura]] states of India.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br/&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br/&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[bn:চ্যালকোপাইরাইট]]&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[bn:চ্যালকোপাইরাইট]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Mukbil</name></author>
	</entry>
	<entry>
		<id>https://en.banglapedia.org/index.php?title=Chalcopyrite&amp;diff=10633&amp;oldid=prev</id>
		<title>Nasirkhan: Content Updated.</title>
		<link rel="alternate" type="text/html" href="https://en.banglapedia.org/index.php?title=Chalcopyrite&amp;diff=10633&amp;oldid=prev"/>
		<updated>2021-06-18T05:52:08Z</updated>

		<summary type="html">&lt;p&gt;Content Updated.&lt;/p&gt;
&lt;table style=&quot;background-color: #fff; color: #202122;&quot; data-mw=&quot;interface&quot;&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 05:52, 18 June 2021&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l1&quot;&gt;Line 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&amp;lt;p class=Normal &amp;gt;&lt;/del&gt;&#039;&#039;&#039;Chalcopyrite&#039;&#039;&#039; ore mineral of copper; crystallises in the tetragonal crystal system, but crystals are generally small with diphenoidal faces resembling the tetrahedron; usually massive with a metallic lustre and brass or golden-yellow colour; shows greenish-black streaks, uneven fracture and indistinct cleavage; hardness is 3.5-4 on Moh&#039;;s scale and specific gravity is 4.1-4.3. Chalcopyrite is also known as copper pyrite or yellow pyrite and because of its physical appearance it is also called &#039;fools&#039;; gold&#039;;. It occurs in mesothermal or hypothermic deposits. The upper part of the Rajmahal Traps has been highly weathered and there is indication of the presence of chalcopyrite and chalcocite in the rocks. However, chalcopyrite is not very stable as it has low hardness as compared to other heavy minerals and as such it is extremely rare in heavy mineral suites of various vertical sections of the Chittagong, Chittagong Hill Tracts and [[surma basin]] of Bangladesh and [[assam]] and [[tripura]] states of India. [Sifatul Quader Chowdhury] [Chowdhury, Sifatul Quader  Professor of Geology, Dhaka University]&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&#039;&#039;&#039;Chalcopyrite&#039;&#039;&#039; ore mineral of copper; crystallises in the tetragonal crystal system, but crystals are generally small with diphenoidal faces resembling the tetrahedron; usually massive with a metallic lustre and brass or golden-yellow colour; shows greenish-black streaks, uneven fracture and indistinct cleavage; hardness is 3.5-4 on Moh&#039;;s scale and specific gravity is 4.1-4.3. Chalcopyrite is also known as copper pyrite or yellow pyrite and because of its physical appearance it is also called &#039;fools&#039;; gold&#039;;. It occurs in mesothermal or hypothermic deposits. The upper part of the Rajmahal Traps has been highly weathered and there is indication of the presence of chalcopyrite and chalcocite in the rocks. However, chalcopyrite is not very stable as it has low hardness as compared to other heavy minerals and as such it is extremely rare in heavy mineral suites of various vertical sections of the Chittagong, Chittagong Hill Tracts and [[surma basin]] of Bangladesh and [[assam]] and [[tripura]] states of India. [Sifatul Quader Chowdhury] [Chowdhury, Sifatul Quader  Professor of Geology, Dhaka University]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br/&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br/&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[bn:চ্যালকোপাইরাইট]]&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[bn:চ্যালকোপাইরাইট]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Nasirkhan</name></author>
	</entry>
	<entry>
		<id>https://en.banglapedia.org/index.php?title=Chalcopyrite&amp;diff=1343&amp;oldid=prev</id>
		<title>0:0:0:0:0:0:0:1: Content Updated.</title>
		<link rel="alternate" type="text/html" href="https://en.banglapedia.org/index.php?title=Chalcopyrite&amp;diff=1343&amp;oldid=prev"/>
		<updated>2021-06-17T19:03:49Z</updated>

		<summary type="html">&lt;p&gt;Content Updated.&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;&amp;lt;p class=Normal &amp;gt;&amp;#039;&amp;#039;&amp;#039;Chalcopyrite&amp;#039;&amp;#039;&amp;#039; ore mineral of copper; crystallises in the tetragonal crystal system, but crystals are generally small with diphenoidal faces resembling the tetrahedron; usually massive with a metallic lustre and brass or golden-yellow colour; shows greenish-black streaks, uneven fracture and indistinct cleavage; hardness is 3.5-4 on Moh&amp;#039;;s scale and specific gravity is 4.1-4.3. Chalcopyrite is also known as copper pyrite or yellow pyrite and because of its physical appearance it is also called &amp;#039;fools&amp;#039;; gold&amp;#039;;. It occurs in mesothermal or hypothermic deposits. The upper part of the Rajmahal Traps has been highly weathered and there is indication of the presence of chalcopyrite and chalcocite in the rocks. However, chalcopyrite is not very stable as it has low hardness as compared to other heavy minerals and as such it is extremely rare in heavy mineral suites of various vertical sections of the Chittagong, Chittagong Hill Tracts and [[surma basin]] of Bangladesh and [[assam]] and [[tripura]] states of India. [Sifatul Quader Chowdhury] [Chowdhury, Sifatul Quader  Professor of Geology, Dhaka University]&lt;br /&gt;
&lt;br /&gt;
[[bn:চ্যালকোপাইরাইট]]&lt;/div&gt;</summary>
		<author><name>0:0:0:0:0:0:0:1</name></author>
	</entry>
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