Thickness of Unconsolidated Sediments in the Eastern Mediterranean Sea

How-Kin Wong, E. F. K. Zarudzki

Geological Society of America Bulletin · 1969 · 60 citations · 0 references

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Research Article| December 01, 1969 Thickness of Unconsolidated Sediments in the Eastern Mediterranean Sea HOW-KIN WONG; HOW-KIN WONG Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543 Search for other works by this author on: GSW Google Scholar EDWARD F. K ZARUDZKI EDWARD F. K ZARUDZKI Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543 Search for other works by this author on: GSW Google Scholar Author and Article Information HOW-KIN WONG Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543 EDWARD F. K ZARUDZKI Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543 Publisher: Geological Society of America Received: 04 Apr 1969 First Online: 02 Mar 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Copyright © 1969, The Geological Society of America, Inc. Copyright is not claimed on any material prepared by U.S. government employees within the scope of their employment. GSA Bulletin (1969) 80 (12): 2611–2614. https://doi.org/10.1130/0016-7606(1969)80[2611:TOUSIT]2.0.CO;2 Article history Received: 04 Apr 1969 First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation HOW-KIN WONG, EDWARD F. K ZARUDZKI; Thickness of Unconsolidated Sediments in the Eastern Mediterranean Sea. GSA Bulletin 1969;; 80 (12): 2611–2614. doi: https://doi.org/10.1130/0016-7606(1969)80[2611:TOUSIT]2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract The unconsolidated sedimentary layer in the eastern Mediterranean Sea becomes more variable in thickness toward the east. The distribution pattern suggests that the primary sources of sediment in Cenozoic times have been the Nile River, elevated areas of Cyrenaica, the Taurus, and the Apennines. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.