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Geostatistical analyses of IODP Hole 339-U1389D
Shipboard core description and thickness measurements were used as base for the current data. These were verified and, where necessary, minor corrections made during re-logging... -
Geostatistical analyses of IODP Hole 339-U1389C
Shipboard core description and thickness measurements were used as base for the current data. These were verified and, where necessary, minor corrections made during re-logging... -
Geostatistical analyses of IODP Hole 339-U1389B
Shipboard core description and thickness measurements were used as base for the current data. These were verified and, where necessary, minor corrections made during re-logging... -
Geostatistical analyses of IODP Hole 339-U1389A
Shipboard core description and thickness measurements were used as base for the current data. These were verified and, where necessary, minor corrections made during re-logging... -
Geostatistical analyses of IODP Hole 339-U1387B
Shipboard core description and thickness measurements were used as base for the current data. These were verified and, where necessary, minor corrections made during re-logging... -
Geostatistical analyses of IODP Hole 339-U1387A
Shipboard core description and thickness measurements were used as base for the current data. These were verified and, where necessary, minor corrections made during re-logging... -
Geostatistical analyses of IODP Hole 339-U1386B
Shipboard core description and thickness measurements were used as base for the current data. These were verified and, where necessary, minor corrections made during re-logging... -
Geostatistical analyses of IODP Hole 339-U1386A
Shipboard core description and thickness measurements were used as base for the current data. These were verified and, where necessary, minor corrections made during re-logging... -
Thickness, age and layers data of sediments at IODP Site U1386, U1387, and U1389
The bi-gradational sequence is recognised as a defining feature of contourite deposition. The present research questions are: In what pattern these bi-gradational sequences are...
