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    <Identification_Area>
        <logical_identifier>urn:nasa:pds:context:investigation:individual.lab_shocked_feldspars</logical_identifier>
        <version_id>1.0</version_id>
        <title>Investigation of Laboratory Shocked Feldspars</title>
        <information_model_version>1.11.0.0</information_model_version>
        <product_class>Product_Context</product_class>
        <Modification_History>
            <Modification_Detail>
                <modification_date>2019-04-22</modification_date>
                <version_id>1.0</version_id>
                <description>Initial version</description>
            </Modification_Detail>
        </Modification_History>
    </Identification_Area>
    <Reference_List>
        <Internal_Reference>
            <lid_reference>urn:nasa:pds:lab_shocked_feldspars:data</lid_reference>
            <reference_type>context_to_associate</reference_type>
        </Internal_Reference>
        <Internal_Reference>
            <lid_reference>urn:nasa:pds:lab_shocked_feldspars:document:laboratory_shocked_plag_microspec</lid_reference>
            <reference_type>context_to_associate</reference_type>
        </Internal_Reference>
        <External_Reference>
            <doi>10.1029/2018JE005523</doi>
            <reference_text>Jaret, S.J., Johnson, J.R., Sims, M., DiFrancesco, N., and Glotch, T.D., Microscopic and petrographic 
                comparison of experimentally shocked albite, andesine, and bytownite, Journal of Geophysical Research, 123, 
                1701-1722, 2018, doi:10.1029/2018JE005523. 
            </reference_text>
        </External_Reference>
    </Reference_List>
    <Investigation>
        <type>Individual Investigation</type>
        <start_date>2015</start_date>
        <stop_date>2018</stop_date>
        <description>This investigation (associated with Jaret et al., 2018) consists of data acquired from thin sections created 
            from a suite of experimentally shocked plagioclase feldspars. The data products comprise (1) micro-Fourier Transform 
            Infrared (FTIR) thermal infrared hyperspectral image cubes; (2) thermal infrared point spectra acquired with two 
            different detectors; (3) micro-Raman spectra; (4) microscope images of the thin sections in plane polarized and cross 
            polarized light; and (5) microscope images of the locations of the Raman and thermal infrared point spectra.  The 
            thermal infrared and Raman spectroscopy demonstrate changes as a function of shock pressure, as detailed in Jaret et 
            al., 2018.</description>
    </Investigation>
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