-
Parent record: Datasets relating to core GC-14, located in the Capricorn...
National Institute of Water and Atmosphere (NIWA)
Core GC14 (23o49' 52S 154o21' 67E) was collected from the Capricorn Channel at a depth of 2004 mbsl (metres below sea level). By investigating the properties and components of... -
Parent record: Datasets relating to core GC13, located in the Capricorn...
National Institute of Water and Atmosphere (NIWA)
Core GC13 (23o47' 30S 154o13' 56E) was collected from the Capricorn Channel at a depth of 1482 mbsl (metres below sea level). By investigating the properties and components of... -
Parent record: Datasets relating to core GC-12, located in the Capricorn...
National Institute of Water and Atmosphere (NIWA)
Core GC12 (23o34' 37S 153o49' 94E) was collected from the Capricorn Channel at a depth of 990.5 mbsl (metres below sea level). By investigating the properties and components of... -
Parent record: Datasets relating to core GC-11, located in the Capricorn...
National Institute of Water and Atmosphere (NIWA)
Core GC11 (23o23' 07S 153o22' 00E) was collected from the Capricorn Channel at a depth of 502 mbsl (metres below sea level). By investigating the properties and components of... -
Parent record: Datasets relating to core GC-10, located in the Capricorn...
National Institute of Water and Atmosphere (NIWA)
Core GC10 (22o59 76S 152o48' 00E) was collected from the Capricorn Channel at a depth of 335 mbsl (metres below sea level). By investigating the properties and components of... -
Parent record: Datasets relating to core GC-09, located in the Capricorn...
National Institute of Water and Atmosphere (NIWA)
Core GC09 (22o53' 70S 152o38' 10E) was collected from the Capricorn Channel at a depth of 166 mbsl (metres below sea level). By investigating the properties and components of... -
Determining main carbonate mineralogy, and the primary components of the non...
National Institute of Water and Atmosphere (NIWA)
A gravity core (GC10) was collected from a depth of 335 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). Analysis of other parameters revealed the Last... -
Determining main carbonate mineralogy, and the primary components of the non...
National Institute of Water and Atmosphere (NIWA)
A gravity core (GC14) was collected from a depth of 2004 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). Analysis of other parameters revealed the Last... -
Determining main carbonate mineralogy, and the primary components of the non...
National Institute of Water and Atmosphere (NIWA)
A gravity core (GC11) was collected from a depth of 502 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). Analysis of other parameters revealed the Last... -
Determining main carbonate mineralogy, and the primary components of the non...
National Institute of Water and Atmosphere (NIWA)
A gravity core (GC13) was collected from a depth of 1482 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). Analysis of other parameters revealed the Last... -
Determining main carbonate mineralogy, and the primary components of the non...
National Institute of Water and Atmosphere (NIWA)
A gravity core (GC09) was collected from a depth of 166m within the Capricorn Channel, southern Great Barrier Reef (GBR). Analysis of other parameters revealed the Last Glacial... -
Determining main carbonate mineralogy, and the primary components of the non...
National Institute of Water and Atmosphere (NIWA)
A gravity core (GC12) was collected from a depth of 990.5 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). Analysis of other parameters revealed the Last... -
AuSEABED
The auSEABED was created by Dr. Chris Jenkins, a former staff member of School of Geoscience, to describe the materials of the Australian Maritime Region - in all, an area...
1 - 13 of 13 results