Article
Environmental Sciences
Zihan Zheng, Yuncheng Cao, Wenyue Xu, Duofu Chen
Summary: The lack of quantification of deep dissolved methane flux in hydrate systems limits our understanding of methane accumulation and distribution. This study proposes a numerical model to quantify the dissolved methane flux based on parameters related to gas bubble distribution. The model is then applied to ODP Site 995 at the Blake Ridge, showing consistent results with seismic data. The study also explores the influence of upward methane flux on hydrate accumulation and provides insights into regional methane flux estimation.
FRONTIERS IN MARINE SCIENCE
(2022)
Article
Geochemistry & Geophysics
Kehua You, Lori Summa, Peter Flemings, Manasij Santra, Yi Fang
Summary: The systematic model presented in this study links the generation, migration, phase partitioning, and accumulation of methane into a closed loop mechanism, controlled by the deposition of coarse-grained layers and the base of hydrate stability zone during sediment burial. This model helps to explore for high-concentration methane hydrate in geological systems and is important for understanding the methane budget and carbon cycle under the seafloor. The coupling of geological evolution, microbial methane generation, and gas flow by buoyancy results in concentrated hydrate deposits at structural closures, illustrating how these factors contribute to the generation of high-concentration methane hydrate.
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
(2021)
Article
Geochemistry & Geophysics
Bin Liu, Li Yang, Jiangxin Chen, Leonardo Azevedo, Tonggang Han
Summary: Pipe structures are considered as critical pathways for fluid migration beneath cold seeps. The investigation of a pipe structure in the Haima cold seep region reveals multiple small-scale gas pockets within the structure, resembling magma chambers beneath volcanoes. Analysis of diffraction waves and numerical seismic modeling supports the hypothesis, providing new insights into gas migration processes within pipe structures.
Article
Geochemistry & Geophysics
Yichuan Wang, Heather Bedle, Kurt J. Marfurt
Summary: Gas hydrate deposits on continental margins have gained global attention. While the bottom-simulating reflector (BSR) is commonly used as an indicator for gas hydrate presence, it is insufficient for identifying and quantifying the hydrates. Therefore, measuring seismic stratigraphic and attenuation attributes is a useful method for characterizing gas hydrates. This approach allows the identification of short-scale layering patterns that provide information about the amount and mechanism of gas hydrates. By using sparse strongest peaks and attenuation parameters Q(-1) and gamma, complete time-variant spectra and spectral differences at different times can be measured. The obtained results from seismic data over the Hikurangi and Gondwana margins in eastern New Zealand show high-quality spectral and attenuation images that correlate with BSRs and provide insights into free-gas and gas-hydrate accumulations.
GEOPHYSICAL JOURNAL INTERNATIONAL
(2023)
Article
Energy & Fuels
Oleg Bazaluk, Kateryna Sai, Vasyl Lozynskyi, Mykhailo Petlovanyi, Pavlo Saik
Summary: Ukraine is heavily dependent on energy resources, especially natural gas, prompting the search for alternative sources such as gas hydrates in the Black Sea. Studies suggest significant hydrate deposits in the region, with refined dissociation parameters being crucial. The development of a 3D visualization model for the dissociation zone and assessment of potential recoverable gas volumes have been successful, providing valuable insights for new technological schemes in gas recovery from the deep-water Black Sea area.
Article
Environmental Sciences
Hui Li, Xuekang Lu, Lin Wang, Wenjing Wang, Tianhua Li, Wanjun Lu, Yong Chen
Summary: Most experiments indicate that gas hydrates are enriched in C2+ gases compared to the feeding gas source, due to fractionation during the crystallization process. However, sediments below the gas hydrate stability zone (BGHSZ) are relatively enriched in C2+ hydrocarbon gases compared to the hydrate-occurring zone above. The mechanisms causing these variations are still unclear. To investigate these mechanisms, a series of pore-scale experimental observations were conducted, simulating the dissolution-migration-hydration processes.
FRONTIERS IN MARINE SCIENCE
(2023)
Article
Geochemistry & Geophysics
Jyoti Sharma, M. Ravi Kumar, Ketan Singha Roy, S. K. Pal, P. N. S. Roy
Summary: The study revealed the presence of intracrustal layers, lid, and a low-velocity zone (LVZ) in the northwestern Deccan volcanic province, showing anisotropic and isotropic variations. The LVZ, which is a negative anomaly, may be related to partial melts, volatile materials, or a thermal anomaly.
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
(2021)
Article
Geosciences, Multidisciplinary
Arka Dyuti Sarkar, Mads Huuse
Summary: Accurate estimation of present-day subsurface temperatures is crucial for the energy industry. By applying the reflection seismic thermometry (RST) process, high-quality seismic data can be used to remotely measure subsurface temperatures at a high spatial resolution. This case study demonstrates the power of RST to provide indicative subsurface temperature results in frontier exploration basins, reducing uncertainty over source rock maturity prior to drilling.
Article
Geochemistry & Geophysics
Jiangong Wei, Tingting Wu, Xiuli Feng, Jinqiang Liang, Wenjing Li, Rui Xie, Gang Wu
Summary: Gas hydrates are potential future energy resources found in marine sediments and permafrost areas. The distribution, saturation, physical properties, and mechanical behavior of gas hydrate-bearing sediments were studied, showing spatial heterogeneity in gas hydrate saturation and varying deviatoric stress and permeability with increasing saturation and burial depth.
Article
Energy & Fuels
Yuanlong Wei, Lingyun Zhao, Wei Liu, Xiong Zhang, Zhijun Guo, Zhangli Wu, Shenghui Yuan
Summary: In this paper, the reservoir parameters of coalbed methane (CBM) in a working area in Western Guizhou Province, China were predicted using 3D seismic exploration technology, and the sweet-spot area was evaluated based on the prediction results. New technologies and methods suitable for CBM were explored, and a quantitative prediction technology of CBM sweet spots was developed. A multi-parameter weighted step-by-step evaluation method based on inversion was proposed for comprehensive evaluation of sweet spots. The C409 coal seam was selected as the sweet spot based on this method.
Article
Geosciences, Multidisciplinary
Hugh Daigle, Yi Fang, Stephen C. Phillips, Peter B. Flemings
Summary: Mercury injection capillary pressure measurements were used to characterize the pore structure of three channel-levee lithofacies from the gas hydrate reservoir in Green Canyon Block 955 in the northern Gulf of Mexico. The results showed that resedimentation is an effective method for recreating intact sample fabric. The pore structure varied across different lithofacies, and the maximum hydrate saturation was controlled by different limitations.
Article
Oceanography
Canping Li, Jiachun You, Yanchun Tan, Fengying Chen, Yilin Liu, Zihao Guo, Xinyu Tian
Summary: This study extracted three amplitude-class attributes from the migration sections of five methane bubble plumes and obtained a linear correlation between gas content and seismic attributes. The results suggest a relatively good correlation between gas content and amplitude attributes, with correlation coefficients close to 1.0. These findings lay a foundation for further estimation of gas content and hydrate reserves based on the distribution of seafloor bubbles.
ACTA OCEANOLOGICA SINICA
(2021)
Article
Geochemistry & Geophysics
Zachary F. M. Burton, Laura N. Dafov
Summary: This study proposes and demonstrates salt movement, particularly diapirism, as a new mechanism for the recycling of marine gas hydrates (GH). The research shows that salt diapir movement can significantly increase GH volumes and saturations. The results suggest that GH systems associated with salt diapir crests are attractive targets for hydrocarbon resource exploration and scientific drilling expeditions.
GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
(2023)
Article
Geosciences, Multidisciplinary
Yu Hu, Min Luo, Joern Peckmann, Xinxin Zhang, Linying Chen, Junxi Feng, Qianyong Liang, Duofu Chen, Dong Feng
Summary: This study analyzes the methods for quantifying the extent of authigenic carbonate formation in marine sediments and proposes a new approach for quantifying this formation in modern and ancient oceans. By analyzing pore-water parameters from areas affected by methane diffusion in the northern South China Sea, a significant positive correlation between carbonate precipitation rate and sulfate flux is found. This finding can be used to quantify the formation of authigenic carbonate in shallow sediments along continental margins and is important for understanding past carbon cycling and its relation to climate.
GEOPHYSICAL RESEARCH LETTERS
(2023)
Article
Geochemistry & Geophysics
Aoshuang Ji, Tieyuan Zhu, Hector Marin-Moreno, Xiong Lei
Summary: This study combines seismic data and rock-physics modeling to investigate the influence of gas-hydrate saturation and morphology on seismic attenuation in hydrate-bearing sediments. The results suggest that seismic attenuation is controlled by both gas-hydrate saturation and morphology, with varying relationships between attenuation and saturation for different hydrate morphologies. Squirt flow, driven by pressure gradients in adjacent pores, may be responsible for significant attenuation variations across a broad frequency range.
INTERPRETATION-A JOURNAL OF SUBSURFACE CHARACTERIZATION
(2021)
Article
Geochemistry & Geophysics
Colton Lynner, Harm J. A. Van Avendonk, Anne Becel, Gail L. Christeson, Brandon Dugan, James B. Gaherty, Steven Harder, Matthew J. Hornbach, Daniel Lizarralde, Maureen D. Long, M. Beatrice Magnani, Donna J. Shillington, Kasey Aderhold, Zachary C. Eilon, Lara S. Wagner
SEISMOLOGICAL RESEARCH LETTERS
(2020)
Article
Geosciences, Multidisciplinary
Jiten Patel, Rupert Sutherland, Michael Gurnis, Harm Van Avendonk, Sean P. S. Gulick, Brandon Shuck, Joann Stock, Erin Hightower
Summary: Solander Basin is characterized by subduction initiation at the Pacific-Australia plate boundary and high biological productivity at the northern edge of the Antarctic Circumpolar Current. Tectonic influences on sedimentary architecture, along with climate influence on ocean currents and biological productivity, have shaped the basin's features.
Article
Geochemistry & Geophysics
Xiaoyu Yuan, Jun Korenaga, W. Steven Holbrook, Peter B. Kelemen
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
(2020)
Article
Geology
Aleasha King, Patrick Lepine, Andrew R. Gorman, David J. Prior, Adrienn Lukacs, Hamish Bowman, Sheng Fan, Andrew Robertson, Franz Lutz, Jennifer D. Eccles, Stefan Buske, Vera Lay, Douglas R. Schmitt, Heather Schijns
Summary: The glacio-fluvial sediments in the Whataroa Valley in New Zealand's South Island provide a record of environmental change since the Last Glacial Maximum, as well as insights into the Alpine Fault's location and characteristics. Analyzing seismic profiles, researchers identified different reflective seismic facies and faults associated with the Alpine Fault.
NEW ZEALAND JOURNAL OF GEOLOGY AND GEOPHYSICS
(2021)
Article
Geochemistry & Geophysics
Nathaniel C. Miller, Daniel Lizarralde, John A. Collins, W. Steven Holbrook, Harm J. A. Van Avendonk
Summary: Seismic anisotropy measurements indicate that upper mantle hydration is limited to serpentinization and/or fault zones, not distributed uniformly, impacting important processes at the Middle America Trench; outer rise plate-bending faults may provide a pathway for seawater to rehydrate the slab mantle; hydration confined to fault zones reduces water storage estimates for the MAT upper mantle.
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
(2021)
Article
Geography, Physical
Greer Gilmer, Christopher M. Moy, Christina R. Riesselman, Marcus Vandergoes, Geraldine Jacobsen, Andrew R. Gorman, Emily J. Tidey, Gary S. Wilson
Summary: The study reconstructs the environmental changes of a fjord ingression basin in the subantarctic Auckland Islands of New Zealand, covering deglacial, lacustrine, marine transgression, and marine stages. The results indicate significant historical events in the Southern Hemisphere in the early 20th century, including glacier retreat, sea-level rise, and environmental changes.
QUATERNARY SCIENCE REVIEWS
(2021)
Article
Geochemistry & Geophysics
Brandon Shuck, Harm Van Avendonk, Sean P. S. Gulick, Michael Gurnis, Rupert Sutherland, Joann Stock, Jiten Patel, Erin Hightower, Steffen Saustrup, Thomas Hess
Summary: The Puysegur margin in the southern New Zealand region has experienced a series of tectonic events over the past 45 million years, transitioning from rifting to strike-slip to incipient subduction. Through deep-penetrating imaging techniques, it has been revealed that subduction initiation in the Puysegur Trench was likely assisted by inherited structural weaknesses imprinted into the lithosphere during earlier continental rifting and strike-slip events. Forced nucleation along a strike-slip boundary is identified as a viable subduction initiation scenario, which has implications for understanding subduction initiation throughout Earth's history.
Article
Geochemistry & Geophysics
Andrew C. Gase, Harm J. A. Van Avendonk, Nathan L. Bangs, Dan Bassett, Stuart A. Henrys, Daniel H. N. Barker, Shuichi Kodaira, Katrina M. Jacobs, Thomas W. Luckie, David A. Okaya, Gou Fujie, Yojiro Yamamoto, Adrien F. Arnulf, Ryuta Arai
Summary: The study explores the crustal structure and accretion dynamics of the northern Hikurangi margin using new seismic data, revealing the significant impact of volcanic cover on seismic reflectivity and variations in frontal prism structure that may be related to different sediment supply or past seamount collisions.
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
(2021)
Article
Geosciences, Multidisciplinary
B. J. Eppinger, J. L. Hayes, B. J. Carr, S. Moon, C. L. Cosans, W. S. Holbrook, C. J. Harman, Z. T. Plante
Summary: Weathering processes can weaken and break apart rock, releasing nutrients and increasing the permeability of subsurface materials. By quantifying seismic anisotropy in weathered materials at different depths, researchers can better understand the effects of weathering on rock fabric and its implications for hydrology, geomorphology, and landscape evolution. The findings suggest a correlation between in situ weathering and anisotropy, indicating that weathering may amplify the intrinsic anisotropy of bedrock.
JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE
(2021)
Article
Geochemistry & Geophysics
G. J. Crutchley, J. J. Mountjoy, J. I. T. Hillman, F. Turco, S. Watson, P. B. Flemings, B. Davy, S. Woelz, A. R. Gorman, J. Bialas
Summary: Research has shown that gas migration through vertical conduits within the gas hydrate stability zone is a global phenomenon, impacting seafloor biodiversity and ocean biogeochemistry. Seismic imaging of the gas hydrate system beneath an anticlinal ridge at New Zealand's Hikurangi subduction margin revealed the accumulation of gas beneath the stability zone, leading to the formation of a vertical gas conduit to the seafloor. The presence of highly reflective zones at the bases of gas conduits suggests the importance of intervening sealing units in determining their formation.
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
(2021)
Article
Geosciences, Multidisciplinary
Dan Bassett, Adrien Arnulf, Stuart Henrys, Dan Barker, Harm Avendonk, Nathan Bangs, Shuichi Kodaira, Hannu Seebeck, Laura Wallace, Andrew Gase, Thomas Luckie, Katie Jacobs, Brook Tozer, Ryuta Arai, David Okaya, Kimi Mochizuki, Gou Fujie, Yojiro Yamamoto
Summary: Marine multichannel and wide-angle seismic data were used to study the crustal structure along a 530 km margin-parallel transect of the Hikurangi subduction zone. The research found that the subducting Hikurangi Plateau crust is about 1 km thicker and has slightly higher mantle velocities beneath the south/central Hikurangi compared to the north Hikurangi. In the overthrusting plate, there is a significant reduction in forearc wavespeeds from south to north, accompanied by a change in seismic reflection character. The study suggests that the geological architecture of the overthrusting plate contributes to spatial variability in the location of shallow frictional transitions along the Hikurangi margin, impacting seismic and tsunami hazard.
GEOPHYSICAL RESEARCH LETTERS
(2022)
Article
Geochemistry & Geophysics
Vera Lay, Stefan Buske, John Townend, Richard Kellett, Martha Savage, Douglas R. Schmitt, Alexis Constantinou, Jennifer D. Eccles, Andrew R. Gorman, Malcolm Bertram, Kevin Hall, Don Lawton, Randolph Kofman
Summary: The Alpine Fault in New Zealand is a crucial transpressional plate boundary which is late in its typical earthquake cycle. A seismic survey in the Whataroa Valley has provided new insights into the subsurface structures of the Alpine Fault zone, revealing the complexity of the tectonic processes at play. Despite challenging conditions, seismic imaging has identified various structures related to the valley and the fault system, deepening our understanding of the geology in the area.
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
(2021)
Article
Water Resources
Brady A. Flinchum, W. Steven Holbrook, Bradley J. Carr
Summary: Fractures in Earth's critical zone affect groundwater flow, storage, and chemical weathering. Seismic velocities in the fractured bedrock layer of the critical zone are scale-dependent, with smaller-scale velocities showing significant heterogeneity in fracture density and larger-scale velocities being slower and lacking lateral heterogeneity. The discrepancy is a result of the contrasting measurement scales between the two methods, providing information on the fractured medium at vastly different scales.
FRONTIERS IN WATER
(2022)
Article
Water Resources
Travis Nielson, John Bradford, W. Steven Holbrook, Mark Seyfried
Summary: In snow-dominated mountainous watersheds in the northern hemisphere, north-facing slopes tend to be more deeply weathered than south-facing slopes due to the more persistent snowpack. A study conducted in Johnston Draw revealed that differences in snow accumulation can lead to variations in weathering depth, with the largest difference occurring where snow accumulation is greatest.
FRONTIERS IN WATER
(2021)