ALBERT

Description: International Ocean Discovery Program (IODP) Site U1517(proposed Site TLC-04B) is located at 38°49.772ʹS, 178°28.557ʹE inthe extensional, creeping part of the Tuaheni Landslide Complex(TLC) (Figure F1; see Figure F2 in the Expedition 372A summarychapter [Barnes et al., 2019a]) (Mountjoy et al., 2014b). HoleU1517A was drilled in a water depth of 725 meters below sea level(mbsl); Holes U1517B and U1517C lie at 720 mbsl. The primarydrilling objective was to log and sample through the landslide massand the gas hydrate stability zone to understand the mechanismsbehind creeping. Therefore, we planned to log the sediment columnto 205 meters below seafloor (mbsf ) using logging-while-drilling(LWD) tools, followed by advanced piston corer (APC) coring, pres-sure coring, and temperature dual pressure probe (T2P) deploy-ments.

Description: Subaqueous slopes are susceptible to a broad range of failure mechanisms and deformation styles, many of which are not well characterised. We undertook novel laboratory-based testing using a Dynamic Back-Pressured Shearbox on samples collected from an area subject to ongoing slope failures, situated on the upper slope of New Zealand's Hikurangi Margin, to determine how increases in pore water and gas pressures generate shallow mass movement. Using both water and nitrogen gas we observed similar responses in both cases, indicating that behaviour is dominated by the normal effective stress state regardless of pore-fluid phase. Shear-strain accumulation, representing landslide movement, shows a slow episodic pattern, in common with many shallow terrestrial landslides. Our results are relevant for landslides occurring in shallow near surface sedimentary sequences but have implications for deep-seated landslide behaviour. They suggest that once movement initiates at a critical effective stress, its rate is regulated through dilation and pore expansion within the shear zone, temporarily increasing effective stress within a narrow shear band and suppressing rapid shear. Consequently, under certain conditions, shallow submarine landslides (e.g. spreading failures) can undergo slow episodic movement which allows them to accumulate large shear strains without accelerating to catastrophic movement even when they are unconstrained.

Description: Highlights • We report on methane seeps found at shallow depths on New Zealand's Hikurangi Margin. • Tools have been applied to measure bubble characteristics from video footage and to estimate the gas flow rate using acoustic data. • We estimate that the entire Tuaheni seep field produces somewhere in the range of 30–2415 t of methane per year. • The density of seeps at this location is far greater than anything else observed on the Hikurangi Margin. Abstract We analyse an area of high density submarine methane gas seeps situated on the shelf to slope transition (130–420 m water depth) on the northern region of New Zealand's Hikurangi margin, off Poverty Bay. Multibeam and singlebeam echo sounder data collected in 2014 and 2015 revealed 〉600 seeps, at much greater density than any previously mapped areas of seepage on the Hikurangi margin. To broadly constrain the output of methane from these seeps, we have estimated the flow of methane at individual seeps, utilising perspective-measurements applied to still frames from a deep towed camera system to measure the dimensions of rising bubbles. We combine bubble size and rise-rate distributions with singlebeam acoustic data to estimate gas flow rates at six selected seeps sites. Our results predict a wide range (3.0–2249 mL/min) of methane release into the water column. If we assume that the six seeps we analysed are representative of the entire seep population, and that gas flow is constant, we can extrapolate across the seep field and infer a gas release of 30 to 2415 t of methane per year into the ocean.