Deutsch
 
Datenschutzhinweis Impressum
  DetailsucheBrowse

Datensatz

DATENSATZ AKTIONENEXPORT
Zur Ablage hinzufügen
  Lokale TagsFreigabegeschichteDetailsÜbersicht

Freigegeben
Konferenzbeitrag

Gas hydrates beneath the Tuaheni Landslide Complex, New Zealand. First results from IODP Expedition 372

Urheber*innen

Pecher,  Ingo
External Organizations (TEMPORARY!);

Barnes,  Philip
External Organizations (TEMPORARY!);

/persons/resource/katjah

Heeschen,  Katja
3.1 Inorganic and Isotope Geochemistry, 3.0 Geochemistry, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Torres ,  Marta
External Organizations (TEMPORARY!);

Cook,  Ann
External Organizations (TEMPORARY!);

Moore,  Gregory
External Organizations (TEMPORARY!);

Dugan,  Brandon
External Organizations (TEMPORARY!);

Mountjoy,  Joshu
External Organizations (TEMPORARY!);

Crutchley,  Gareth
External Organizations (TEMPORARY!);

Expedition 372&375 Scientific Party, 
External Organizations (TEMPORARY!);

Externe Ressourcen
Volltexte (frei zugänglich)
Es sind keine frei zugänglichen Volltexte in GFZpublic verfügbar
Ergänzendes Material (frei zugänglich)
Es sind keine frei zugänglichen Ergänzenden Materialien verfügbar
Zitation

Pecher, I., Barnes, P., Heeschen, K., Torres, M., Cook, A., Moore, G., Dugan, B., Mountjoy, J., Crutchley, G., Expedition 372&375 Scientific Party (2018): Gas hydrates beneath the Tuaheni Landslide Complex, New Zealand. First results from IODP Expedition 372, (Geophysical Research Abstracts ; Vol. 20, EGU2018-4221-1, 2018), General Assembly European Geosciences Union (Vienna, Austria 2018), 4221-1-4221-1.


Zitierlink: https://gfzpublic.gfz-potsdam.de/pubman/item/item_3149896
Zusammenfassung
The Tuaheni Landslide Complex (TLC) on the Hikurangi Margin was drilled during IODP Expedition 372 with logging-while-drilling (LWD) and coring at Site U1517. The TLC is slowly deforming (“creeping”) and, based on seismic images, known to be underlain by gas hydrates. The overarching goal at U1517 was to establish if and how hydrates are linked to creeping. We logged 205 m beneath the seafloor (mbsf) with LWD and achieved almost full core recovery down to 190 mbsf, below the base of the gas hydrate stability zone. We constrained gas hydrate saturation from LWD data, mainly based on resistivity and sonic velocities. Gas hydrate saturation was also determined from Cl- anomalies in samples that were selected immediately after coring using infrared images. We here present first results from this expedition.