ᴡʜᴀᴛ ᴍɪɴᴇʀᴀʟꜱ ᴡᴏᴜʟᴅ ʏᴏᴜ ᴇxᴘᴇᴄᴛ ᴛᴏ ꜰɪɴᴅ ɪɴ ᴛʜᴇ ꜰᴏʟʟᴏᴡɪɴɢ ʀᴏᴄᴋꜱ? ʙᴀꜱᴀʟᴛ - __________________________________________________________ ________________________________________________________________ ₁. ᴅɪᴏʀɪᴛᴇ - _________________________________________________________ ________________________________________________________________ ₂. ɢʀᴀɴɪᴛᴇ - _________________________________________________________ ________________________________________________________________ ₃. ɢᴀʙʙʀᴏ- _________________________________________________________ ________________________________________________________________ ʏᴏᴜ ʜᴀᴠᴇ ᴀ ᴍᴀɢᴍᴀ ᴛʜᴀᴛ ɪꜱ ᴀᴛ ᴠᴇʀʏ ʜɪɢʜ ᴛᴇᴍᴘᴇʀᴀᴛᴜʀᴇ ᴀɴᴅ ᴘʀᴇꜱꜱᴜʀᴇ. ᴡʜᴀᴛ ᴍɪɴᴇʀᴀʟꜱ ᴡᴏᴜʟᴅ ʙᴇ ᴘʀᴇꜱᴇɴᴛ ɪɴ ᴛʜᴇ ʀᴏᴄᴋ ᴛʜᴀᴛ ᴡᴏᴜʟᴅ ꜰᴏʀᴍ ꜰʀᴏᴍ ᴛʜɪꜱ ᴍᴀɢᴍᴀ ɪꜰ ɪᴛ ꜱᴏʟɪᴅɪꜰɪᴇᴅ Qᴜɪᴄᴋʟʏ ɪɴꜱɪᴅᴇ ᴛʜᴇ ᴇᴀʀᴛʜ (ɪɴᴛʀᴜꜱɪᴠᴇ)? ᴡʜʏ?

Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
icon
Related questions
Question

ᴀᴄᴛɪᴠɪᴛʏ ₉: ʙᴏᴡᴇɴ’ꜱ ʀᴇᴀᴄᴛɪᴏɴ ꜱᴇʀɪᴇꜱ
ᴅɪʀᴇᴄᴛɪᴏɴꜱ: ᴜꜱᴇ ᴛʜᴇ ᴅɪᴀɢʀᴀᴍ ᴛᴏ ᴀɴꜱᴡᴇʀ ᴛʜᴇ ꜰᴏʟʟᴏᴡɪɴɢ Qᴜᴇꜱᴛɪᴏɴꜱ ᴛʜᴀᴛ ꜰᴏʟʟᴏᴡ.

₁. ᴡʜᴀᴛ ᴍɪɴᴇʀᴀʟꜱ ᴡᴏᴜʟᴅ ʏᴏᴜ ᴇxᴘᴇᴄᴛ ᴛᴏ ꜰɪɴᴅ ɪɴ ᴛʜᴇ ꜰᴏʟʟᴏᴡɪɴɢ ʀᴏᴄᴋꜱ?
ʙᴀꜱᴀʟᴛ - __________________________________________________________
________________________________________________________________


₁. ᴅɪᴏʀɪᴛᴇ - _________________________________________________________
________________________________________________________________
₂. ɢʀᴀɴɪᴛᴇ - _________________________________________________________
________________________________________________________________
₃. ɢᴀʙʙʀᴏ- _________________________________________________________
________________________________________________________________

ʏᴏᴜ ʜᴀᴠᴇ ᴀ ᴍᴀɢᴍᴀ ᴛʜᴀᴛ ɪꜱ ᴀᴛ ᴠᴇʀʏ ʜɪɢʜ ᴛᴇᴍᴘᴇʀᴀᴛᴜʀᴇ ᴀɴᴅ ᴘʀᴇꜱꜱᴜʀᴇ. ᴡʜᴀᴛ ᴍɪɴᴇʀᴀʟꜱ ᴡᴏᴜʟᴅ
ʙᴇ ᴘʀᴇꜱᴇɴᴛ ɪɴ ᴛʜᴇ ʀᴏᴄᴋ ᴛʜᴀᴛ ᴡᴏᴜʟᴅ ꜰᴏʀᴍ ꜰʀᴏᴍ ᴛʜɪꜱ ᴍᴀɢᴍᴀ ɪꜰ ɪᴛ ꜱᴏʟɪᴅɪꜰɪᴇᴅ Qᴜɪᴄᴋʟʏ ɪɴꜱɪᴅᴇ ᴛʜᴇ
ᴇᴀʀᴛʜ (ɪɴᴛʀᴜꜱɪᴠᴇ)? ᴡʜʏ?

Rock Texture
BOWEN'S REACTION SERIES
BOWEN'S REACTION SERIES
Calcium
Aphanitic
Phaneritic
Unstable
at 1 bar
Formed at
High
Ca, Mg. Fe Temperature Minerals
Low Olivine
Silica
Contains
High
Plagioclase
Olivine
Calcium
Plagioclase
&
25 C
(surface
conditions)
Pryoxene
Basalt
Gabbro
Pressure
Pryoxene
Amphibole
Andesite
Diorite
Amphibole
Biotite
Sodium
Biotite
Sodium
Plagioclase
Potassium Feldspar
Muscovite
Quartz
Plagioclase
Trachyte
Syenite (w/o quartz)
Potassium Feldspar
Muscovite
Quartz
High
(w. quartz)
More
Low
Rhyolite
Granite
High
K, Na, Si Temperature
Silica
Stable
Pressure
Transcribed Image Text:Rock Texture BOWEN'S REACTION SERIES BOWEN'S REACTION SERIES Calcium Aphanitic Phaneritic Unstable at 1 bar Formed at High Ca, Mg. Fe Temperature Minerals Low Olivine Silica Contains High Plagioclase Olivine Calcium Plagioclase & 25 C (surface conditions) Pryoxene Basalt Gabbro Pressure Pryoxene Amphibole Andesite Diorite Amphibole Biotite Sodium Biotite Sodium Plagioclase Potassium Feldspar Muscovite Quartz Plagioclase Trachyte Syenite (w/o quartz) Potassium Feldspar Muscovite Quartz High (w. quartz) More Low Rhyolite Granite High K, Na, Si Temperature Silica Stable Pressure
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