Arabia–Eurasia collision and the forcing of mid-Cenozoic global cooling

2008/05/10 by Mark B. Allen, Howard A. Armstrong · 6 citations
Earth and Planetary Sciences · #Geological and Geochemical Analysis #Geology and Paleoclimatology Research #earthquake and tectonic studies

paper · doi:10.1016/j.palaeo.2008.04.021

openalex publication_date 2008/05/10 · crossref created 2008/05/10 · crossref issued 2008/07/01 · crossref published 2008/07/01 · crossref published-print 2008/07/01 · crossref deposited 2018/12/28 · openalex created_date 2025/10/10 · crossref indexed 2026/07/30 · openalex updated_date 2026/07/30

Citations

• Phanerozoic geodynamic evolution of northeastern Africa and the northwestern Arabian platform
• New evidence and solution to the Maden complex controversy of the Southeast Anatolian orogenic belt (Turkey)
• Rapid Cenozoic glaciation of Antarctica induced by declining atmospheric CO2
• Trends, Rhythms, and Aberrations in Global Climate 65 Ma to Present
• Biogeographic responses to geodynamics: A key study all around the Oligo–Miocene Tethyan Seaway
• The Saghand Region, Central Iran: U-Pb geochronology, petrogenesis and implications for Gondwana Tectonics

Cited by

• The vertical separation of mainshock rupture and microseismicity at Qeshm island in the Zagros fold-and-thrust belt, Iran
• The Role of Carbon Dioxide During the Onset of Antarctic Glaciation
• 40Ar/39Ar dating of Quaternary lavas in northwest Iran: constraints on the landscape evolution and incision rates of the Turkish-Iranian plateau
• The role of eastern Tethys seaway closure in the Middle Miocene Climatic Transition (ca. 14 Ma)
• Cenozoic [wikipedia]
• Oligocene [wikipedia]