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
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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
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
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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