clay and quartz
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
Related questions
Question
chosen options are wrong
![What minerals usually remain after intense weathering
of silicate rocks such as granite?
olivine and hornblende
quartz and calcite
obsidian and feldspar
clay and calcite
clay and quartz](/v2/_next/image?url=https%3A%2F%2Fcontent.bartleby.com%2Fqna-images%2Fquestion%2F4d4321a5-4dfd-4eec-a3eb-8a39051ceb96%2Feb68d959-ff50-45de-b288-148d0ee4f076%2Feggcu9_processed.jpeg&w=3840&q=75)
Transcribed Image Text:What minerals usually remain after intense weathering
of silicate rocks such as granite?
olivine and hornblende
quartz and calcite
obsidian and feldspar
clay and calcite
clay and quartz
![Geologists cannot date a clastic sedimentary rock
directly using isotopic geochronologic methods. Why
not?
those rocks do not contain the appropriate radio-
isotopes
those rocks do not contain the appropriate minerals
dates would indicate the times the minerals
weathered out of the parent materials rather than
depositional age
dates would indicate the times the minerals formed
in igneous or metamorphic rocks rather than
depositional age
the isotopic half-lives are too short](/v2/_next/image?url=https%3A%2F%2Fcontent.bartleby.com%2Fqna-images%2Fquestion%2F4d4321a5-4dfd-4eec-a3eb-8a39051ceb96%2Feb68d959-ff50-45de-b288-148d0ee4f076%2Fugc4o7_processed.jpeg&w=3840&q=75)
Transcribed Image Text:Geologists cannot date a clastic sedimentary rock
directly using isotopic geochronologic methods. Why
not?
those rocks do not contain the appropriate radio-
isotopes
those rocks do not contain the appropriate minerals
dates would indicate the times the minerals
weathered out of the parent materials rather than
depositional age
dates would indicate the times the minerals formed
in igneous or metamorphic rocks rather than
depositional age
the isotopic half-lives are too short
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