Southeastern Section..............................................................................................6 Northeast Section.....................................................................................................6 Announcements In Me
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چکیده
IS SN 0 03 209 19 Editor: Marshall D. Sundberg Department of Biological Sciences Emporia State University 1200 Commercial Street, Emporia, KS 66801-5707 Telephone: 620-341-5605 Fax: 620-341-5607 Email: [email protected] Th e B ot an ic al So ci et y o f A m er ic a: T he So ci et y f or A LL Pl an t B io lo gi sts Metasequoia Musings..............................................................................................................2
منابع مشابه
Nannostratigraphy and paleoenvironmental study of the lower boundary of the Kalat Formation in East and West of Kopeh- Dagh, Northeast Iran
This study presents the nannostratigraphy and nannofossil events in the lower boundary of Kalat Formation in the East and West of the Kopeh- Dagh basin. The Kalat Formation comprises of coarse grained detritus limestone with subordinate sandstone intercalations. In the current study, six sections have been chosen in the East and West of the basin which are as follow: Dobaradar section, Kalat se...
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The Tirgan Formation (Barremian – Aptian) is exposed in the Kopet Dagh in northeast Iran. One stratigraphic section in Zavin was measured with a thickness of 110 meters. This Formation in section consists of three parts (including lower carbonate, limy shale – marl and upper carbonate rocks). Based on the study of 94 thin sections, 10 carbonate and 2 siliciclastic lithofacies have been identifi...
متن کاملBiostratigraphy and paleo-ecological reconstruction on Scleractinian reef corals of Rupelian-Chattian succession (Qom Formation) in northeast of Delijan area
In this research, biostratigraphy and paleo-ecological reconstruction of the Qom Formation deposits in Bijegan village, northeast ofDelijan, are discussed. The studied section is situated in the western margin of the Urumieh-Dokhtar magmatic arc (the intra-arc basin).The Qom Formation deposits at the studied area are Rupelian-Chattian in age. Larger benthic foraminifers are used for biostratigr...
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Contributions to the Development of Soil MicrobiolSocieties, and Meetings: ogy from the Southeastern United States: DR. F. The Virginia Academy of Science: DR. SIDNEY S. B. SMITH . 95 NEGUS. The Southeastern Section of the Botanical The American Federation for Clinical Research: DR. Society of America: DR. KENNETH W. HUNT ...... 115 MAURICE A. SCHNITKER ..98........................................
متن کاملThermobarometry and mineral chemistry of Central Iran Permo-Triassic lamprophyres in Chahrisseh Region, northeast Isfahan
Chahrisseh magmatic rocks are located in the northeast Isfahan, in the Sanandaj-Sirjan structural zone and parallel to the Qom-Zefre fault. These magmatic masses are located in a continuous section of Permian-Triassic sediments and rarely enter the Early Triassic beds. These rocks contain anhydrous ferromagnesium minerals (olivine, clinopyroxene and plagioclase), hydrous ferromagnesium minerals...
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