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The geometry and architecture of a well exposed syn-rift normal fault array in the Suez rift is examined.
Traditional fabrication techniques have limitations in controlling the geometry and architecture of the electrode and solid-state electrolytes, which would otherwise compromise the performance.
Here, we examine the geometry and architecture of the Jezero western delta fluvial stratigraphy using high-resolution orbital images and digital elevation models (DEMs).
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In this paper, we review the dimensions, geometry and architecture of the components of the Kalahari Craton and the various positions this important crustal block could have occupied within Rodinia.
This chapter discusses the role of the channel geometry and architecture of large pore zeolites FAU, BEA, and MOR on the activity, selectivity, and time-on-stream stability in trimethylbenzene transalkylation with toluene to xylenes.
Electrical resistivity soundings were used to map the large-scale geometry and architecture of the palaeochannel system.
TGS technique is best suitable for reservoirs where the lithotypes occur in a sequential order and it helps in defining the geometry and internal architecture of the reservoir rocks (Armstrong et al. 2003).
This morphostructural setting can be comprised in a model, where the tilted and faulted-blocks (inner platform) and stepped margin (outer platform) paleo-topography, inherited from the rifting tectonics, was the most important factor controlling the geometry and depositional architecture of a carbonate platform growing on the Southern Tethyan passive margin.
These various "styles" are essentially facies of mineralization, each one being the product of a particular set of conditions that control the ore-forming processes and the consequent geometry and architecture (style) of the deposits.
Defining the 3D geometry and internal architecture of reservoirs is important for prediction of hydrocarbon volumes, petroleum production and storage potential.
We report the structural geometry and facies architecture of a small diapir-related carbonate-dominated basin from the Jurassic rift of the Moroccan High Atlas.
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