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	<title><![CDATA[Mandakini Study Institute - Patna: Magmatism and Tectonics]]></title>
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	<guid isPermaLink="true">https://kuntal.org/msipstudentslogin/index.php/pages/view/926/magmatism-and-tectonics</guid>
	<pubDate>Fri, 16 Jan 2026 12:19:23 +0000</pubDate>
	<link>https://kuntal.org/msipstudentslogin/index.php/pages/view/926/magmatism-and-tectonics</link>
	<title><![CDATA[Magmatism and Tectonics]]></title>
	<description><![CDATA[<h2 data-end="28" data-start="0">Magmatism and Tectonics</h2><h3 data-end="101" data-start="29">Inter-relationship between Tectonic Settings and Igneous Rock Suites</h3><h3 data-end="119" data-start="103">Introduction</h3><p data-end="519" data-start="120"><strong data-end="147" data-start="120">Magmatism and tectonics</strong> are closely interrelated processes reflecting the thermal and dynamic state of the Earth&rsquo;s interior. Different <strong data-end="280" data-start="259">tectonic settings</strong> control the <strong data-end="375" data-start="293">source of magma, melting mechanism, magma composition and style of emplacement</strong>, resulting in characteristic <strong data-end="428" data-start="405">igneous rock suites</strong>. Hence, specific igneous associations can be used to interpret past tectonic environments.</p><hr data-end="524" data-start="521"><h2 data-end="581" data-start="526">1. Divergent Plate Boundaries (Constructive Margins)</h2><h3 data-end="603" data-start="583">Tectonic Setting</h3><ul data-end="693" data-start="604">
	<li data-end="646" data-start="604">
	<p data-end="646" data-start="606">Mid-ocean ridges and continental rifts</p>
	</li>
	<li data-end="693" data-start="647">
	<p data-end="693" data-start="649">Lithosphere undergoes extension and thinning</p>
	</li>
</ul><h3 data-end="715" data-start="695">Magma Generation</h3><ul data-end="778" data-start="716">
	<li data-end="778" data-start="716">
	<p data-end="778" data-start="718"><strong data-end="743" data-start="718">Decompression melting</strong> of upwelling asthenospheric mantle</p>
	</li>
</ul><h3 data-end="803" data-start="780">Igneous Rock Suites</h3><ul data-end="877" data-start="804">
	<li data-end="827" data-start="804">
	<p data-end="827" data-start="806"><strong data-end="827" data-start="806">Tholeiitic basalt</strong></p>
	</li>
	<li data-end="846" data-start="828">
	<p data-end="846" data-start="830">Gabbro, dolerite</p>
	</li>
	<li data-end="877" data-start="847">
	<p data-end="877" data-start="849">Sheet dykes and pillow lavas</p>
	</li>
</ul><h3 data-end="898" data-start="879">Characteristics</h3><ul data-end="991" data-start="899">
	<li data-end="932" data-start="899">
	<p data-end="932" data-start="901">Low K₂O, low volatile content</p>
	</li>
	<li data-end="965" data-start="933">
	<p data-end="965" data-start="935">Dominantly mafic composition</p>
	</li>
	<li data-end="991" data-start="966">
	<p data-end="991" data-start="968">Forms new oceanic crust</p>
	</li>
</ul><h3 data-end="1004" data-start="993">Example</h3><ul data-end="1061" data-start="1005">
	<li data-end="1027" data-start="1005">
	<p data-end="1027" data-start="1007">Mid-Atlantic Ridge</p>
	</li>
	<li data-end="1061" data-start="1028">
	<p data-end="1061" data-start="1030">East African Rift (continental)</p>
	</li>
</ul><hr data-end="1066" data-start="1063"><h2 data-end="1123" data-start="1068">2. Convergent Plate Boundaries (Destructive Margins)</h2><h3 data-end="1155" data-start="1125">(a) Ocean&ndash;Ocean Subduction</h3><h4 data-end="1178" data-start="1157">Magma Generation</h4><ul data-end="1241" data-start="1179">
	<li data-end="1241" data-start="1179">
	<p data-end="1241" data-start="1181"><strong data-end="1197" data-start="1181">Flux melting</strong> due to addition of H₂O from subducting slab</p>
	</li>
</ul><h4 data-end="1267" data-start="1243">Igneous Rock Suites</h4><ul data-end="1340" data-start="1268">
	<li data-end="1290" data-start="1268">
	<p data-end="1290" data-start="1270">Island-arc tholeiite</p>
	</li>
	<li data-end="1320" data-start="1291">
	<p data-end="1320" data-start="1293">Andesite, basaltic andesite</p>
	</li>
	<li data-end="1340" data-start="1321">
	<p data-end="1340" data-start="1323">Diorite, tonalite</p>
	</li>
</ul><h4 data-end="1362" data-start="1342">Characteristics</h4><ul data-end="1411" data-start="1363">
	<li data-end="1389" data-start="1363">
	<p data-end="1389" data-start="1365">Calc-alkaline affinity</p>
	</li>
	<li data-end="1411" data-start="1390">
	<p data-end="1411" data-start="1392">Enrichment in LILEs</p>
	</li>
</ul><h4 data-end="1425" data-start="1413">Example</h4><ul data-end="1439" data-start="1426">
	<li data-end="1439" data-start="1426">
	<p data-end="1439" data-start="1428">Mariana Arc</p>
	</li>
</ul><hr data-end="1444" data-start="1441"><h3 data-end="1480" data-start="1446">(b) Ocean&ndash;Continent Subduction</h3><h4 data-end="1503" data-start="1482">Magma Generation</h4><ul data-end="1561" data-start="1504">
	<li data-end="1561" data-start="1504">
	<p data-end="1561" data-start="1506">Partial melting of mantle wedge + crustal contamination</p>
	</li>
</ul><h4 data-end="1587" data-start="1563">Igneous Rock Suites</h4><ul data-end="1667" data-start="1588">
	<li data-end="1614" data-start="1588">
	<p data-end="1614" data-start="1590"><strong data-end="1614" data-start="1590">Calc-alkaline series</strong></p>
	</li>
	<li data-end="1643" data-start="1615">
	<p data-end="1643" data-start="1617">Andesite, dacite, rhyolite</p>
	</li>
	<li data-end="1667" data-start="1644">
	<p data-end="1667" data-start="1646">Granodiorite, granite</p>
	</li>
</ul><h4 data-end="1689" data-start="1669">Characteristics</h4><ul data-end="1773" data-start="1690">
	<li data-end="1728" data-start="1690">
	<p data-end="1728" data-start="1692">Intermediate to felsic composition</p>
	</li>
	<li data-end="1751" data-start="1729">
	<p data-end="1751" data-start="1731">High water content</p>
	</li>
	<li data-end="1773" data-start="1752">
	<p data-end="1773" data-start="1754">Explosive volcanism</p>
	</li>
</ul><h4 data-end="1787" data-start="1775">Example</h4><ul data-end="1805" data-start="1788">
	<li data-end="1805" data-start="1788">
	<p data-end="1805" data-start="1790">Andes Mountains</p>
	</li>
</ul><hr data-end="1810" data-start="1807"><h3 data-end="1849" data-start="1812">(c) Continent&ndash;Continent Collision</h3><h3 data-end="1871" data-start="1851">Tectonic Setting</h3><ul data-end="1927" data-start="1872">
	<li data-end="1927" data-start="1872">
	<p data-end="1927" data-start="1874">Thickened crust, high pressure&ndash;temperature conditions</p>
	</li>
</ul><h3 data-end="1949" data-start="1929">Magma Generation</h3><ul data-end="1994" data-start="1950">
	<li data-end="1994" data-start="1950">
	<p data-end="1994" data-start="1952">Partial melting of lower continental crust</p>
	</li>
</ul><h3 data-end="2019" data-start="1996">Igneous Rock Suites</h3><ul data-end="2053" data-start="2020">
	<li data-end="2037" data-start="2020">
	<p data-end="2037" data-start="2022">S-type granites</p>
	</li>
	<li data-end="2053" data-start="2038">
	<p data-end="2053" data-start="2040">Leucogranites</p>
	</li>
</ul><h3 data-end="2066" data-start="2055">Example</h3><ul data-end="2087" data-start="2067">
	<li data-end="2087" data-start="2067">
	<p data-end="2087" data-start="2069">Himalayan granites</p>
	</li>
</ul><hr data-end="2092" data-start="2089"><h2 data-end="2134" data-start="2094">3. Intraplate (Within-Plate) Settings</h2><h3 data-end="2168" data-start="2136">(a) Hotspots (Mantle Plumes)</h3><h4 data-end="2191" data-start="2170">Magma Generation</h4><ul data-end="2219" data-start="2192">
	<li data-end="2219" data-start="2192">
	<p data-end="2219" data-start="2194">Deep mantle plume melting</p>
	</li>
</ul><h4 data-end="2245" data-start="2221">Igneous Rock Suites</h4><ul data-end="2313" data-start="2246">
	<li data-end="2264" data-start="2246">
	<p data-end="2264" data-start="2248">Alkaline basalts</p>
	</li>
	<li data-end="2291" data-start="2265">
	<p data-end="2291" data-start="2267">Tholeiitic flood basalts</p>
	</li>
	<li data-end="2313" data-start="2292">
	<p data-end="2313" data-start="2294">Trachyte, phonolite</p>
	</li>
</ul><h4 data-end="2335" data-start="2315">Characteristics</h4><ul data-end="2371" data-start="2336">
	<li data-end="2371" data-start="2336">
	<p data-end="2371" data-start="2338">Enriched in incompatible elements</p>
	</li>
</ul><h4 data-end="2386" data-start="2373">Examples</h4><ul data-end="2430" data-start="2387">
	<li data-end="2407" data-start="2387">
	<p data-end="2407" data-start="2389">Hawaiian Islands</p>
	</li>
	<li data-end="2430" data-start="2408">
	<p data-end="2430" data-start="2410">Deccan Traps (India)</p>
	</li>
</ul><hr data-end="2435" data-start="2432"><h3 data-end="2467" data-start="2437">(b) Continental Rift Zones</h3><h4 data-end="2485" data-start="2469">Magma Types</h4><ul data-end="2533" data-start="2486">
	<li data-end="2504" data-start="2486">
	<p data-end="2504" data-start="2488">Alkaline basalts</p>
	</li>
	<li data-end="2519" data-start="2505">
	<p data-end="2519" data-start="2507">Carbonatites</p>
	</li>
	<li data-end="2533" data-start="2520">
	<p data-end="2533" data-start="2522">Kimberlites</p>
	</li>
</ul><h4 data-end="2555" data-start="2535">Characteristics</h4><ul data-end="2600" data-start="2556">
	<li data-end="2579" data-start="2556">
	<p data-end="2579" data-start="2558">High alkali content</p>
	</li>
	<li data-end="2600" data-start="2580">
	<p data-end="2600" data-start="2582">Deep mantle source</p>
	</li>
</ul><h4 data-end="2614" data-start="2602">Example</h4><ul data-end="2634" data-start="2615">
	<li data-end="2634" data-start="2615">
	<p data-end="2634" data-start="2617">East African Rift</p>
	</li>
</ul><hr data-end="2639" data-start="2636"><h2 data-end="2687" data-start="2641">4. Ophiolite Suites (Ancient Oceanic Crust)</h2><h3 data-end="2709" data-start="2689">Tectonic Setting</h3><ul data-end="2762" data-start="2710">
	<li data-end="2762" data-start="2710">
	<p data-end="2762" data-start="2712">Obducted oceanic lithosphere at convergent margins</p>
	</li>
</ul><h3 data-end="2792" data-start="2764">Typical Rock Association</h3><ul data-end="2873" data-start="2793">
	<li data-end="2814" data-start="2793">
	<p data-end="2814" data-start="2795">Peridotite (mantle)</p>
	</li>
	<li data-end="2823" data-start="2815">
	<p data-end="2823" data-start="2817">Gabbro</p>
	</li>
	<li data-end="2837" data-start="2824">
	<p data-end="2837" data-start="2826">Sheet dykes</p>
	</li>
	<li data-end="2853" data-start="2838">
	<p data-end="2853" data-start="2840">Pillow basalt</p>
	</li>
	<li data-end="2873" data-start="2854">
	<p data-end="2873" data-start="2856">Pelagic sediments</p>
	</li>
</ul><h3 data-end="2886" data-start="2875">Example</h3><ul data-end="2945" data-start="2887">
	<li data-end="2912" data-start="2887">
	<p data-end="2912" data-start="2889">Semail Ophiolite (Oman)</p>
	</li>
	<li data-end="2945" data-start="2913">
	<p data-end="2945" data-start="2915">Indian ophiolites (Naga Hills)</p>
	</li>
</ul>]]></description>
	<dc:creator>MSIPATNA</dc:creator>
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