Isolating detrital and diagenetic signals in magnetic susceptibility records from methane‐bearing marine sediments
Volume‐dependent magnetic susceptibility (κ) is commonly used for paleoenvironmental
reconstructions in both terrestrial and marine sedimentary environments where it reflects a …
reconstructions in both terrestrial and marine sedimentary environments where it reflects a …
Diagenesis of magnetic minerals in active/relict methane seep: Constraints from rock magnetism and mineralogical records from Bay of Bengal
In this study, we conducted a comprehensive investigation of rock magnetic, mineralogical,
and sedimentological records of sediment cores supplemented by a high resolution seismic …
and sedimentological records of sediment cores supplemented by a high resolution seismic …
Diagenetic dissolution, maghemitization and sulphidization of magnetic minerals in rapidly deposited gas hydrate bearing sediments from the Bay of Bengal
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 …
electron microscopy analyses on a 148.8 m sediment core (NGHP-01-20A) from the …
Diagenetic analysis of shallow and deep-seated gas hydrate systems from the Bay of Bengal
This is the first systematic high-resolution rock magnetic study complemented by
mineralogical and petrological observations conducted on sediment cores representing …
mineralogical and petrological observations conducted on sediment cores representing …
Studies of the Earth's Magnetic Field from Peninsular India: Contributions from CSIR-NGRI
M Venkateshwarlu, K Arora - Journal of the Geological Society of India, 2021 - Springer
Studies of the geomagnetic field and paleomagnetic phenomena were among the earliest
disciplines of geophysics, which were launched in CSIR-NGRI since the early 1960s. Many …
disciplines of geophysics, which were launched in CSIR-NGRI since the early 1960s. Many …
Gas in Marine Sediments (GIMS): past, current, and future (contributions from GIMS-14)
Background Shallow sediment (< 1000 m below the seafloor) along modern continental
margins hosts enormous quantities of low molecular weight hydrocarbons (mostly methane …
margins hosts enormous quantities of low molecular weight hydrocarbons (mostly methane …