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Through continuous development and a clear focus on professional audio/video products, Roland is committed to providing unique solutions to improve workflow and maximize creative possibilities. Roland has introduced many innovative products to the professional market over the past few years and has built a strong trust across many users and installations around the world. Pseudo-overconsolidation is present near the seafloor and is underlain by underconsolidation at depth at some NGHP-01 locations.2 Bringing Professional Audio and Video Together Welcome to the Roland Professional Audio and Video Equipment catalog.

Index properties corroborate more advanced consolidation and triaxial strength test results and can be used for predicting behavior in other NGHP-01 regions. Grain size and porosity effects on permeability are critical, both locally to trap gas and regionally to provide fluid flow to hydrate reservoirs.


Extrapolation of properties from one location to another also enhances our understanding of gas-hydrate reservoir systems. However, comparison of marine and permafrost-related Arctic reservoirs provides insight into the inter-relationships and common traits between physical properties and the morphology of gas-hydrate reservoirs regardless of location. Properties of individual NGHP-01 wells and regional trends are discussed in detail. The presence of hydrate in conjunction with other geologic processes may be responsible for sediment porosity being nearly uniform for almost 500 m off the Andaman Islands. However, even in these fine-grained sediments, gas hydrate preferentially forms in coarser sediment or fractures, when present. Coarser-grained reservoirs (permafrost-related and marine) may contain high gas-hydrate-pore saturations, while finer-grained reservoirs may contain low-saturation disseminated or more complex gas-hydrates, including nodules, layers, and high-angle planar and rotational veins. Properties from the hydrate-free Kerala-Konkan basin off the west coast of India are also presented. In this paper, the physical properties of hydrate-bearing regions offshore eastern India (Krishna-Godavari and Mahanadi Basins) and the Andaman Islands, determined from Expedition NGHP-01 cores, are compared to each other, well logs, and published results of other hydrate reservoirs. The presence and type of gas, porewater chemistry, fluid migration, and subbottom temperature may govern the hydrate formation process, but it is the host sediment that commonly dictates final hydrate habit, and whether hydrate may be economically developed. The sediment characteristics of hydrate-bearing reservoirs profoundly affect the formation, distribution, and morphology of gas hydrate.
