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One of the owners of (720) 201-4650 is between 20-30 years old. We have records for 2 possible previous addresses for the owner, 3 other possible phone numbers, and 3 possible related persons connected to this individual.
Mesostructural, Isotopic and Geochemical Constraints on the Brittle Tectonic Evolution of the LA Spezia Region, Northwest Apennines, Italy. (Ph.D. Dissertation)• Documented the Evolution of Fracture Systems and Tectonic Fluids During Late Extensional Deformation Phase in the LA Spezia Region of the Northern Apennines Thrust Belt (Nw Italy)• Created A Regional Structural Interpretation That Demonstrated the Tectonic Evolution from Continental Collision That Produced the Thrust Belt, Overprinted by Rift Tectonics. • Determined the Connectivity of Tectonic Fault-Related Fluid Reservoir(S) Using Multiple Isotopic Tracers (Strontium, Oxygen and Carbon), with Which the Interaction History of Host Rocks and Tectonic Fluids was Modeled• Developed A Framework of Detailed 1:2,500 Scale Computer-Based Geologic Maps of Tectonic Veins, Faults and Fractures to Describe Fracture/Fluid Interactions and Fluid/Fracture Evolution Over A 15 Km2 Area Show Less
Structural Analysis Across the Northeast Boundary of the Taconic Allochthon, West-Central Vermont (M.S. Thesis)• Constrained the Timing of Taconic Allochthon Emplacement and Subsequent Thrust Imbrication by Analyzing Changes in Structural Features (Cleavage and Fault Generations) Across the Basal Thrust of the Taconic Allochthon (Pelitic Strata) Into the Underlying Parautochthonous Carbonate Shelf Strata• Documented Using Field Mapping Integrated and Thin-Section Petrographic Analysis the Complex Regional Structural Sequence and Mesostructural and Microstructural Characteristics of Five Overprinting Tectonic Deformation Phase Show Less
Strain Analysis and Slaty Cleavage in the Taconic Slate Belt, West-Central Vermont (B.A. Thesis)Evaluated the Strain State Along-Strike of the Taconic Allochthon in the Taconic Slate Belt of West-Central Vermont Using Diagenetic Reduction Spots Found in the Slates as Strain Indicators
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