300°C 600°C 900°C Subduction zone: Subducting sediments and seafloor basalt are metamorphosed due to increase in pressur

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300°C 600°C 900°C Subduction zone: Subducting sediments and seafloor basalt are metamorphosed due to increase in pressur

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300 C 600 C 900 C Subduction Zone Subducting Sediments And Seafloor Basalt Are Metamorphosed Due To Increase In Pressur 1
300 C 600 C 900 C Subduction Zone Subducting Sediments And Seafloor Basalt Are Metamorphosed Due To Increase In Pressur 1 (52.66 KiB) Viewed 13 times
300 C 600 C 900 C Subduction Zone Subducting Sediments And Seafloor Basalt Are Metamorphosed Due To Increase In Pressur 2
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300°C 600°C 900°C Subduction zone: Subducting sediments and seafloor basalt are metamorphosed due to increase in pressure of subducting plate and increasing temperature with depth -100 km 200 km © 2012 Pearson Education, Inc Volcanic (magmatic) arc: Shallow crustal rocks are metamorphosed by heat from rising magma Subducting oceanic lithosphere Igneous intrusions Match the appropriate letter (W-Z) with the metamorphic facies (assemblage of minerals) based on relative temperature and pressure. (In the answer box, enter the number 1-4).
Match the appropriate letter (W-Z) with the metamorphic facies (assemblage of minerals) based on relative temperature and pressure. (In the answer box, enter the number 1-4). amphibolite facies (low pressure, high temp) blueschist facies (high pressure, low temp) eclogite facies (high pressure, high temp) greenschist facies (low pressure, low temp) 1. W 2. X 3. Y 4. Z
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