Deformation and Gravity Change: Indicators of Isostasy, Tectonics, Volcanism, and Climate Change /
| Corporate Author: | |
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| Other Authors: | , |
| Format: | eBook |
| Language: | English |
| Published: |
Basel :
Birkhäuser Basel : Imprint: Birkhäuser,
2007.
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| Edition: | 1st ed. 2007. |
| Series: | Pageoph Topical Volumes,
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| Subjects: |
Table of Contents:
- Deformation and Gravity Change: Indicators of Isostasy, Tectonics, Volcanism and Climate Change. Introduction
- An Overview of the Small BAseline Subset Algorithm: A DInSAR Technique for Surface Deformation Analysis
- Propagator-matrix Technique for the Viscoelastic Response of a Multi-layered Sphere to Surface Toroidal Traction
- Using Fuzzy Logic for the Analysis of Sea-level Indicators with Respect to Glacial-isostatic Adjustment: An Application to the Richmond-Gulf Region, Hudson Bay
- Shear-wave Velocity Structure around Teide Volcano: Results Using Microtremors with the SPAC Method and Implications for Interpretation of Geodetic Results
- Steric Sea-level Variations Inferred from Combined Topex/Poseidon Altimetry and GRACE Gravimetry
- Interpretation of 1992-1994 Gravity Changes around Mayon Volcano, Philippines, Using Point Sources
- Glacial-isostatic Adjustment and the Viscosity Structure Underlying the Vatnajökull Ice Cap, Iceland
- Review of Microgravity Observations at Mt. Etna: A Powerful Tool to Monitor and Study Active Volcanoes
- An Estimate of Global Mean Sea-level Rise Inferred from Tide-gauge Measurements Using Glacial-isostatic Models Consistent with the Relative Sea-level Record
- Modeling of Stress Changes at Mayon Volcano, Philippines
- A Hybrid Model for the Summit Region of Merapi Volcano, Java, Indonesia, Derived from Gravity Changes and Deformation Measured between 2000 and 2002
- Vertical Crustal Motion along the Mediterranean and Black Sea Coast Derived from Ocean Altimetry and Tide Gauge Data
- Some Insights into Topographic, Elastic and Self-gravitation Interaction in Modelling Ground Deformation and Gravity Changes in Active Volcanic Areas.