Authigenic greigite may form at any time within a sediment during diagenesis. Its formation
pathway, timing of formation, and geological preservation potential are key to resolving the …

Understanding the locus of fluid flow along thrust and splay faults is important to understand
the hydraulic properties of accretionary systems and fault mechanics. Here, we use rock …

Authigenic ferrimagnetic iron sulfides, essentially greigite (Fe3S4), are commonly found in
gas hydrate-bearing marine sediments of active accretionary prisms. Greigite is a by …

Diagenetically formed magnetic minerals at marine methane seep sites are potential archive
of past fluid flow and could provide important constraints on the evolution of past methane …

This is the first systematic high-resolution rock magnetic study complemented by
mineralogical and petrological observations conducted on sediment cores representing …

Thermomagnetic analysis is performed by bringing subject materials into its cooled and
heated state, followed by analyzing the magnetic moment change. Performing these would …

Accurately determining the solubility of ethane in oil‐based mud is crucial for assessing the
severity of gas kicks and implementing appropriate well control procedures. The key factors …

We conducted a detailed rock magnetic study complemented by sedimentological and
mineralogical methods on a 177.2-m-long sediment core of Hole NGHP-01-14A to constrain …

We conducted a comprehensive rock magnetic investigation complemented by a scanning
electron microscopy analyses on a 148.8 m sediment core (NGHP-01-20A) from the …

Few investigations of iron speciation exist in intertidal conditions with little attention given to
understanding the geochemical behavior of Fe 3+–Fe 2+ and its biogeochemical processes …