Hongdan Deng
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View article: Incongruent melting of garnet during garnet-spinel transition and its implication to the lithospheric exhumation
Incongruent melting of garnet during garnet-spinel transition and its implication to the lithospheric exhumation Open
Phase transition of garnet-spinel is one of the major parameters affecting the lithosphere dynamics. The transition processes of garnet to spinel, however, remain unclear. Spinel-pyroxene symplectites around garnet from one olivine-webster…
View article: Reconciling patterns of long-term topographic growth with coseismic uplift by synchronous duplex thrusting
Reconciling patterns of long-term topographic growth with coseismic uplift by synchronous duplex thrusting Open
How long-term changes in surface topography relate to coseismic uplift is key to understanding the creation of high elevations along active mountain fronts, and remains hotly debated. Here we investigate this link by modeling the developme…
View article: CCDC 2277772: Experimental Crystal Structure Determination
CCDC 2277772: Experimental Crystal Structure Determination Open
An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available …
View article: Crust necking of the northeastern South China Sea: Insights from deep seismic data
Crust necking of the northeastern South China Sea: Insights from deep seismic data Open
During rifting, continental crust necks, leading to significant thickness reduction in a few tens of kilometres. However, deformations associated with the necking process remain elusive due to few outcrop examples and a lack of seismic dat…
View article: “V”型共轭走滑断裂：特征、形成机制及其对青藏高原东南缘晚新生代变形的启示
“V”型共轭走滑断裂：特征、形成机制及其对青藏高原东南缘晚新生代变形的启示 Open
摘要: "V"型共轭走滑断裂是指共轭角为钝角的共轭走滑断裂,其"V"型开口方向为锐角且指示最大拉伸方向.前人开展了大量关于"V"型共轭走滑断裂发育背景及动力学机制的研究,但是目前未有针对"V"型共轭断裂几何学、运动学有关的综述.归纳已有"V"型共轭走滑断裂的几何学、运动学特征,总结现存的"V"型共轭走滑断裂的动力学机制,并选取青藏高原东南缘"V"型共轭走滑断裂,进行实例分析.分布于美国西部、欧亚板块中西部和西藏中部的"V"型共轭走滑断裂特征揭示共轭角大小与断裂滑动速率及断裂…
View article: Influence of paleo-uplift on structural deformation of salt-bearing fold-and-thrust belt: Insights from physical modeling
Influence of paleo-uplift on structural deformation of salt-bearing fold-and-thrust belt: Insights from physical modeling Open
Paleo-uplift is one of the main controlling factors that influence the style of deformation in salt-bearing fold-and-thrust belt (FTB). Whereas, how paleo-uplift amplitude influences salt-related deformations in FTB remains unclear. Here w…
View article: Three-dimensional geometry and growth of a basement-involved fault network developed during multiphase extension, Enderby Terrace, North West Shelf of Australia
Three-dimensional geometry and growth of a basement-involved fault network developed during multiphase extension, Enderby Terrace, North West Shelf of Australia Open
<div>Basement fault reactivation, and the growth, interaction, and linkage with new fault segments are fundamentally three-dimensional and critical for understanding the evolution of fault network development in sedimentary basins. T…
View article: Supplemental Material: Three-dimensional geometry and growth of a basement-involved fault network developed during multiphase extension, Enderby Terrace, North West Shelf of Australia
Supplemental Material: Three-dimensional geometry and growth of a basement-involved fault network developed during multiphase extension, Enderby Terrace, North West Shelf of Australia Open
Figures S1–S3.
View article: Supplemental Material: Three-dimensional geometry and growth of a basement-involved fault network developed during multiphase extension, Enderby Terrace, North West Shelf of Australia
Supplemental Material: Three-dimensional geometry and growth of a basement-involved fault network developed during multiphase extension, Enderby Terrace, North West Shelf of Australia Open
Figures S1–S3.
View article: South China Sea documents the transition from wide continental rift to continental break up
South China Sea documents the transition from wide continental rift to continental break up Open
During extension, the continental lithosphere thins and breaks up, forming either wide or narrow rifts depending on the thermo-mechanical state of the extending lithosphere. Wide continental rifts, which can reach 1,000 km across, have bee…