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• Fake email addresses - Malicious actors sometimes send from email addresses made to look like an official email address but in fact is missing a letter(s), misspelled, replaces a letter with a lookalike number (e.g. “O” and “0”), or originates from free email services that would not be used for official communications.
Phishing scams happen when you receive an email that looks like it came from a company you trust (like AOL), but is ultimately from a hacker trying to get your information. All legitimate AOL Mail will be marked as either Certified Mail, if its an official marketing email, or Official Mail, if it's an important account email. If you get an ...
Learn how to report spam and other abusive conduct.
Reviews of Geophysics is a quarterly peer-reviewed scientific journal published by Wiley-Blackwell on behalf of the American Geophysical Union. The current editor-in-chief is Fabio Florindo ( National Institute of Geophysics and Volcanology –Rome).
Born in Ardahan, Turkey, Yılmaz graduated from Haydarpasha Lyceum in Istanbul and went on to earn a BS in geology with geophysics option from the University of Missouri-Rolla. [2] He earned an MS in 1972 from Stanford University working on rock physics. [3] After five years in the oil and gas industry, he earned his PhD from Stanford in 1979.
Nigel Allister Anstey (born 1927) [1] is a British geophysicist who has made major contributions to seismic exploration, which are the foundations for many of the techniques used in today's oil and gas exploration. Anstey's contributions impact every major area of seismic exploration -– from seismic acquisition to seismic processing to ...
Stephen E. "Steve" Haggerty (born 1938) is an American geophysicist and Fulbright scholar. [1] He served as a principal investigator in the U.S. Apollo and the Soviet Luna sample return programs. The metallic mineral known as " haggertyite " is named in his honor.
In the area of geophysics, we recently developed a theory for the migration of subglacial lakes under ice sheets and earthquake dislocations moving at a transonic velocity on a fault separating rock of sightly different elastic constants.In the area of geophysics, our primary research area is in the theory of the flow of glaciers and ice sheets.