Zobrazeno 1 - 10
of 2 189
pro vyhledávání: '"pore fluid"'
Autor:
S. A. Williams, M. E. French
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 10, Pp n/a-n/a (2024)
Abstract Dilatant hardening is one proposed mechanism that causes slow earthquakes along faults. Previous experiments and models show that dilatant hardening can stabilize fault rupture and slip in several lithologies. However, few studies have syste
Externí odkaz:
https://doaj.org/article/7510f5ca7e01422d9bc3b341870cb05b
Publikováno v:
矿业科学学报, Vol 8, Iss 6, Pp 744-757 (2023)
The Lower Shihezi Formation in the eastern part of Sulige gas field has high water content, where the exploitation of tight sandstone gas reservoir is considerably affected by the characteristics of fluid occurrence. Specifically, this study analyzed
Externí odkaz:
https://doaj.org/article/166c17d6d140498d8e755241fce98c19
Autor:
Raffaella DeMatteis, Bruno Massa, Guido Maria Adinolfi, Ortensia Amoroso, Toshiko Terakawa, Vincenzo Convertito
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 6, Pp n/a-n/a (2024)
Abstract Induced seismicity represents a negative drawback during subsurface exploitation for geothermal energy production. Understanding the triggering mechanisms of induced earthquakes can help implement effective seismic hazard mitigation actions.
Externí odkaz:
https://doaj.org/article/1f955010209a4890838669752e965316
Autor:
Lanlan Yao, Zhengming Yang, Haibo Li, Tiyao Zhou, Yapu Zhang, Ning Wang, Meng Du, Qianhui Huang, Xinliang Chen, Huan Meng
Publikováno v:
Frontiers in Earth Science, Vol 12 (2024)
In order to identify and evaluate reservoir wettability, so as to select suitable mining methods to improve oil recovery, wettability evaluation through one-dimensional (1D) and two-dimensional (2D) nuclear magnetic resonance (NMR) technology combine
Externí odkaz:
https://doaj.org/article/6e390cd6f6674c2e98b20bde758c0f0a
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 1, Pp n/a-n/a (2024)
Abstract Pore fluids are ubiquitous throughout the lithosphere and are commonly invoked as the cause of induced seismicity and slow earthquakes. We perform lab experiments to address these questions for drained fault conditions and low pore pressure.
Externí odkaz:
https://doaj.org/article/505453ce8c484a2f98ad01c090f88501
Autor:
Randolph T. Williams
Publikováno v:
Earth, Planets and Space, Vol 75, Iss 1, Pp 1-4 (2023)
Abstract A recent paper by Nishiyama et al. (Earth, Planets, and Space 73:126) examined syntectonic quartz veins to constrain temporal variations in the recurrence intervals between slow slip and tremor events. The authors claim that by examining the
Externí odkaz:
https://doaj.org/article/760066ed47084075bf7154af59ef25ca
Autor:
Jared Suchan, Shahid Azam
Publikováno v:
Geotechnics, Vol 2, Iss 3, Pp 754-764 (2022)
Saline conditions govern soil behavior during evaporation, thereby affecting the water budget in semi-arid regions. This research examined the effects of saline pore fluid on soil behavior during evaporation. The results indicated volumetric reductio
Externí odkaz:
https://doaj.org/article/e0640cba39c94af6b9d3d9a73c395172
Autor:
Gaozhi Liu, Chongbin Zhao
Publikováno v:
Minerals, Vol 13, Iss 11, p 1428 (2023)
Skarn-hosted deposits are commonly recognized as the consequence of magma intrusion within the Earth’s upper crust. The Ergu Pb-Zn deposit can be regarded as a typical skarn-hosted deposit in the hydrothermal ore-forming system within the central L
Externí odkaz:
https://doaj.org/article/8a9e60ec93534a03bd016d99edc2d64f
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