How have northern Hikurangi Margin gravity flow processes evolved in the past 42 ka? Insights from IODP Expedition 372B/375, Site U1520.

Summary

How have northern Hikurangi Margin gravity flow processes evolved in the past 42 ka? Insights from IODP Expedition 372B/375, Site U1520. is a master's thesis^[1].

Key Facts

• How have northern Hikurangi Margin gravity flow processes evolved in the past 42 ka? Insights from IODP Expedition 372B/375, Site U1520. authored Anthony Shorrock^[2].
• How have northern Hikurangi Margin gravity flow processes evolved in the past 42 ka? Insights from IODP Expedition 372B/375, Site U1520.'s instance of is recorded as master's thesis^[3].
• How have northern Hikurangi Margin gravity flow processes evolved in the past 42 ka? Insights from IODP Expedition 372B/375, Site U1520.'s publisher is recorded as ResearchSpace@Auckland^[4].
• How have northern Hikurangi Margin gravity flow processes evolved in the past 42 ka? Insights from IODP Expedition 372B/375, Site U1520.'s country of origin is recorded as New Zealand^[5].
• How have northern Hikurangi Margin gravity flow processes evolved in the past 42 ka? Insights from IODP Expedition 372B/375, Site U1520.'s publication date is recorded as +2021-00-00T00:00:00Z^[6].
• How have northern Hikurangi Margin gravity flow processes evolved in the past 42 ka? Insights from IODP Expedition 372B/375, Site U1520.'s main subject is recorded as Earth science^[7].
• How have northern Hikurangi Margin gravity flow processes evolved in the past 42 ka? Insights from IODP Expedition 372B/375, Site U1520.'s Handle ID is recorded as 2292/56303^[8].
• How have northern Hikurangi Margin gravity flow processes evolved in the past 42 ka? Insights from IODP Expedition 372B/375, Site U1520.'s title is recorded as How have northern Hikurangi Margin gravity flow processes evolved in the past 42 ka? Insights from IODP Expedition 372B/375, Site U1520.^[9].
• How have northern Hikurangi Margin gravity flow processes evolved in the past 42 ka? Insights from IODP Expedition 372B/375, Site U1520.'s copyright holder is recorded as Anthony Shorrock^[10].
• How have northern Hikurangi Margin gravity flow processes evolved in the past 42 ka? Insights from IODP Expedition 372B/375, Site U1520.'s thesis submitted to is recorded as University of Auckland^[11].
• How have northern Hikurangi Margin gravity flow processes evolved in the past 42 ka? Insights from IODP Expedition 372B/375, Site U1520.'s on focus list of Wikimedia project is recorded as NZThesisProject^[12].
• How have northern Hikurangi Margin gravity flow processes evolved in the past 42 ka? Insights from IODP Expedition 372B/375, Site U1520.'s copyright status is recorded as copyrighted^[13].
• How have northern Hikurangi Margin gravity flow processes evolved in the past 42 ka? Insights from IODP Expedition 372B/375, Site U1520.'s online access status is recorded as closed user group^[14].
• How have northern Hikurangi Margin gravity flow processes evolved in the past 42 ka? Insights from IODP Expedition 372B/375, Site U1520.'s thesis committee member is recorded as Lorna J. Strachan^[15].
• How have northern Hikurangi Margin gravity flow processes evolved in the past 42 ka? Insights from IODP Expedition 372B/375, Site U1520.'s thesis committee member is recorded as Helen Bostock^[16].

Body

Designation and Status

How have northern Hikurangi Margin gravity flow processes evolved in the past 42 ka? Insights from IODP Expedition 372B/375, Site U1520.'s instance of is recorded as master's thesis^[3].