Similar Papers

Paper Title
Journal
Date
Author
Deep-Sea Tephra from the Azores during the past 300,000 Years: Eruptive Cloud Height and Ash Volume Estimates
T C Huang ... L Wilson
GSA Bulletin | VOL. 90
T C Huang, et. al.T C Huang ... L Wilson
01 Feb 1979
Deep sea tephra from Nisyros Island, eastern Aegean Sea, Greece
J C Hardiman
Geological Society, London, Special Publications | VOL. 161
J C HardimanJ C Hardiman
01 Jan 1998
Disaster debris estimation using high-resolution polarimetric stereo-SAR
Christian N Koyama ... Motoyuki Sato
ISPRS Journal of Photogrammetry and Remote Sensing | VOL. 120
Christian N Koyama, et. al.Christian N Koyama ... Motoyuki Sato
16 Sep 2016
Effects of the Tarif Number/Diameter Relationship on Volume and Height Estimates
Gary W Clendenen
Western Journal of Applied Forestry | VOL. 5
Gary W ClendenenGary W Clendenen
01 Jan 1990
View more papers

More From: Geological Society of America Bulletin

Paper Title
Journal
Date
Author
Ultra-high temperatures recorded in parental magmas from hybrid zones
Carmen Rodríguez ... Noah Scahmuells
Geological Society of America Bulletin | VOL. -
Carmen Rodríguez, et. al.Carmen Rodríguez ... Noah Scahmuells
03 Feb 2025
Natural evidence of organic nanostructure transformation of shale during bedding-parallel slip
Hongjian Zhu ... Yu Qi
Geological Society of America Bulletin | VOL. -
Hongjian Zhu, et. al.Hongjian Zhu ... Yu Qi
30 Jan 2025
Influence of internal fluid driving mechanisms on red bed bleaching in the Paradox Basin (Colorado Plateau, Utah and Colorado, USA)
Dolan Lucero ... Mark Person
Geological Society of America Bulletin | VOL. -
Dolan Lucero, et. al.Dolan Lucero ... Mark Person
30 Jan 2025
Multiepisode subduction of a mid-oceanic ridge: Insights from West Junggar, southern Central Asian Orogenic Belt
Ji’En Zhang ... Yulong Zhao
Geological Society of America Bulletin | VOL. -
Ji’En Zhang, et. al.Ji’En Zhang ... Yulong Zhao
30 Jan 2025
View more papers

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.