Deformation bands in sandstone: a review
Deformation bands are the most common strain localization feature found in deformed
porous sandstones and sediments, including Quaternary deposits, soft gravity slides and …
porous sandstones and sediments, including Quaternary deposits, soft gravity slides and …
Transition of accretionary wedge structures around the up-dip limit of the seismogenic subduction zone
The Nankai accretionary prism is divided into three segments: outer and inner wedges and
their transition zone. These wedges reflect different aspects of wedge taper, internal …
their transition zone. These wedges reflect different aspects of wedge taper, internal …
The last 2 Myr of accretionary wedge construction in the central Hikurangi margin (North Island, New Zealand): Insights from structural modeling
Three depth‐converted and geologically interpreted seismic profiles provide a clear image
of the offshore outer accretionary wedge associated with oblique subduction of the Pacific …
of the offshore outer accretionary wedge associated with oblique subduction of the Pacific …
Multiple causes of diagenetic fabric anisotropy in weakly consolidated mud, Nankai accretionary prism, IODP Expedition 316
KL Milliken, RM Reed - Journal of Structural Geology, 2010 - Elsevier
In the Nankai accretionary prism and its associated slope sediments early (pre-lithification)
mechanical modification of mud induces preferred alignments of elongate or platy particles …
mechanical modification of mud induces preferred alignments of elongate or platy particles …
Structure and lithology of the Japan Trench subduction plate boundary fault
Abstract The 2011 Mw9. 0 Tohoku‐oki earthquake ruptured to the trench with maximum
coseismic slip located on the shallow portion of the plate boundary fault. To investigate the …
coseismic slip located on the shallow portion of the plate boundary fault. To investigate the …
[HTML][HTML] The role of protothrusts in frontal accretion and accommodation of plate convergence, Hikurangi subduction margin, New Zealand
Protothrusts mark the onset of deformation at the toe of large subduction accretionary
wedges. They are recognized in seismic reflection sections as small-displacement (tens of …
wedges. They are recognized in seismic reflection sections as small-displacement (tens of …
Expedition 349 summary
C.-F. Li, J. Lin, DK Kulhanek, T. Williams, R. Bao, A. Briais, EA Brown, Y. Chen, PD Clift, FS
Colwell, KA Dadd, W.-W. Ding, I. Hernández-Almeida, X.-L. Huang, S. Hyun, T. Jiang, AAP …
Colwell, KA Dadd, W.-W. Ding, I. Hernández-Almeida, X.-L. Huang, S. Hyun, T. Jiang, AAP …
Interactions between deformation and fluids in the frontal thrust region of the NanTroSEIZE transect offshore the Kii Peninsula, Japan: Results from IODP Expedition …
Integrated Ocean Drilling Program (IODP) Expedition 316 Sites C0006 and C0007
examined the deformation front of the Nankai accretionary prism offshore the Kii Peninsula …
examined the deformation front of the Nankai accretionary prism offshore the Kii Peninsula …
Initiation of a thrust fault revealed by analog experiments
To reveal in detail the process of initiation of a thrust fault, we conducted analog experiments
with dry quartz sand using a high-resolution digital image correlation technique to identify …
with dry quartz sand using a high-resolution digital image correlation technique to identify …
[PDF][PDF] 断裂在纯净砂岩中的变形机制及断裂带内部结构
付晓飞， 肖建华， 孟令东 - 吉林大学学报: 地球科学版, 2014 - xuebao.jlu.edu.cn
以纯净砂岩为对象, 考虑了影响断裂变形的主要因素, 包括成岩阶段, 孔隙度, 温度和围压,
系统剖析了不同性质砂岩的断裂变形机制, 微构造特征及形成断裂带的内部结构 …
系统剖析了不同性质砂岩的断裂变形机制, 微构造特征及形成断裂带的内部结构 …