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Khoury, Hani N. (1986) The origin of tripoli in Jordan. Sedimentary Geology, 48 (3) 223-235 doi:10.1016/0037-0738(86)90031-x

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Reference TypeJournal (article/letter/editorial)
TitleThe origin of tripoli in Jordan
JournalSedimentary Geology
AuthorsKhoury, Hani N.Author
Year1986 (July)Volume48
Issue3
PublisherElsevier BV
DOIdoi:10.1016/0037-0738(86)90031-xSearch in ResearchGate
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Mindat Ref. ID548629Long-form Identifiermindat:1:5:548629:2
GUID0
Full ReferenceKhoury, Hani N. (1986) The origin of tripoli in Jordan. Sedimentary Geology, 48 (3) 223-235 doi:10.1016/0037-0738(86)90031-x
Plain TextKhoury, Hani N. (1986) The origin of tripoli in Jordan. Sedimentary Geology, 48 (3) 223-235 doi:10.1016/0037-0738(86)90031-x
In(1986, July) Sedimentary Geology Vol. 48 (3) Elsevier BV

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Khoury, Hani N. (1987) Tripolization of chert in Jordan. Sedimentary Geology, 53 (3) 305-310 doi:10.1016/0037-0738(87)90039-x
Khoury, Hani N. (1986) Depositional environment and diagenesis of the lower part of the Kurnub Sandstone Formation (lower cretaceous), Mahis area, Jordan. Sedimentary Geology, 49 (1) 129-141 doi:10.1016/0037-0738(86)90018-7
(1986) Contents. Sedimentary Geology, 48 (3) 321 doi:10.1016/0037-0738(86)90035-7
(1986) Editorial Board. Sedimentary Geology, 48 (1) doi:10.1016/0037-0738(86)90077-1
Barr, S.M. (1986) Pyroclastic Rocks. Sedimentary Geology, 49 (3) 294 doi:10.1016/0037-0738(86)90045-x
(1986) Contents. Sedimentary Geology, 47 (3) 321 doi:10.1016/0037-0738(86)90091-6
Nielson, Jamie, Kocurek, Gary (1986) Climbing Zibars of the Algodones. Sedimentary Geology, 48 (1) 1-15 doi:10.1016/0037-0738(86)90078-3
Flood, P.G., Walbran, P.D. (1986) A siliciclastic coastal Sabkha, capricorn coast, Queensland, Australia. Sedimentary Geology, 48 (3) 169-181 doi:10.1016/0037-0738(86)90028-x
(1986) Contents. Sedimentary Geology, 49 (3) 307-308 doi:10.1016/0037-0738(86)90056-4
(1986) Introduction. Sedimentary Geology, 51 (1) 1-3 doi:10.1016/0037-0738(86)90021-7
(1983) Editorial Board. Sedimentary Geology, 34 (1) doi:10.1016/0037-0738(83)90031-3
 
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