<?xml version="1.0" encoding="UTF-8" standalone="no"?>

<?xml-model href="https://pds.nasa.gov/pds4/pds/v1/PDS4_PDS_1J00.sch" schematypens="http://purl.oclc.org/dsdl/schematron"?>

<Product_Observational xmlns="http://pds.nasa.gov/pds4/pds/v1" 
  xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" 
  xsi:schemaLocation="http://pds.nasa.gov/pds4/pds/v1 https://pds.nasa.gov/pds4/pds/v1/PDS4_PDS_1J00.xsd">
  <Identification_Area>
    <logical_identifier>urn:nasa:pds:clementine1_gravity_and_topography:gravity_data:thickgrd</logical_identifier>
    <version_id>1.0</version_id>
    <title>Clementine 1: 2-D Grid of Crustal Thickness (One Degree)</title>
    <information_model_version>1.19.0.0</information_model_version>
    <product_class>Product_Observational</product_class>
    <Modification_History>
      <Modification_Detail>
        <modification_date>2023-02-12</modification_date>
        <version_id>1.0</version_id>
        <description>PDS4 migrated product.</description>
      </Modification_Detail>
    </Modification_History>
  </Identification_Area>
  <Observation_Area>
    <Time_Coordinates>
      <start_date_time xsi:nil="true" nilReason="inapplicable"></start_date_time>
      <stop_date_time xsi:nil="true" nilReason="inapplicable"></stop_date_time>
    </Time_Coordinates>
    <Investigation_Area>
      <name>Deep Space Program Science Experiment</name>
      <type>Mission</type>
      <Internal_Reference>
        <lid_reference>urn:nasa:pds:context:investigation:mission.deep_space_program_science_experiment</lid_reference>
        <reference_type>data_to_investigation</reference_type>
        <comment>Clementine 1</comment>
      </Internal_Reference>
    </Investigation_Area>
    <Observing_System>
      <Observing_System_Component>
        <name>Clementine 1</name>
        <type>Host</type>
        <Internal_Reference>
          <lid_reference>urn:nasa:pds:context:instrument_host:spacecraft.clem1</lid_reference>
          <reference_type>is_instrument_host</reference_type>
        </Internal_Reference>
      </Observing_System_Component>
      <Observing_System_Component>
        <name>Radio Science Subsystem</name>
        <type>Instrument</type>
        <Internal_Reference>
          <lid_reference>urn:nasa:pds:context:instrument:clem1.rss</lid_reference>
          <reference_type>is_instrument</reference_type>
        </Internal_Reference>
      </Observing_System_Component>
    </Observing_System>
    <Target_Identification>
      <name>Moon</name>
      <type>Satellite</type>
      <Internal_Reference>
        <lid_reference>urn:nasa:pds:context:target:satellite.earth.moon</lid_reference>
        <reference_type>data_to_target</reference_type>
      </Internal_Reference>
    </Target_Identification>
  </Observation_Area>
  <Reference_List>
    <Internal_Reference>
      <lid_reference>urn:nasa:pds:clementine1_gravity_and_topography:gravity_map:thickgrd_img</lid_reference>
      <reference_type>data_to_associate</reference_type>
    </Internal_Reference>
  </Reference_List>

  <File_Area_Observational>
    <File>
      <file_name>thickgrd.dat</file_name>
      <records>6480</records>
      <comment>
        This file contains a digital,
        1 X 1 degree resolution grid of the crustal thickness of the
        Moon.  It is a 360 X 180 grid from 89.5 to -89.5 degrees
        latitude, and 0.5 to 359.5 degrees longitude.  The array values
        are crustal thickness in kilometers.  A complete Bouguer
        correction was applied to the lunar gravity field, using the
        newly derived topography from Clementine.  Additional corrections
        were applied for the added mass of mare basalts, using the
        thicknesses given for eight major basins in Solomon and Head
        (Reviews of Geophysics, v. 18, p. 107-141, 1980).  The resulting
        Bouguer anomalies were then inverted for the topography of the
        lunar moho (Mohorovicic Discontinuity), assuming a constant
        density crust (2800 kg/m3) and mantle (3300 kg/m3).  The
        difference between the inferred moho topography and the surface
        topography is referred to as the crustal thickness.  Smooth
        downward continuation of the Bouguer anomalies to a 61 km mean
        depth to the moho matches the 55 km crustal thickness obtained at
        the Apollo 12 and 14 landind sites.
        
        The file contains 180 blocks of 36 records each, with each 
        record containing 10 crustal thickness values plus an ASCII 
        carriage-return line-feed pair as a delimiter.  The first block
        contains values at -89.5 latitude; the first value in the first 
        record is the crustal thickness at (-89.5, 0.5).
      </comment>
    </File>
    
    <Stream_Text>
      <offset unit="byte">0</offset>
      <parsing_standard_id>7-Bit ASCII Text</parsing_standard_id>
      <description>
        This is a 2-D grid of the crustal thickness of the Moon in 
        kilometers
      </description>
      <record_delimiter>Carriage-Return Line-Feed</record_delimiter>
    </Stream_Text>
  </File_Area_Observational>

  <File_Area_Observational_Supplemental>
    <File>
      <file_name>thickgrd.lbl</file_name>
    </File>
    <Stream_Text>
      <offset unit="byte">0</offset>
      <parsing_standard_id>PDS3</parsing_standard_id>
      <description>Original PDS3 label</description>
      <record_delimiter>Carriage-Return Line-Feed</record_delimiter>
    </Stream_Text>
  </File_Area_Observational_Supplemental>
</Product_Observational>
