NEW DATA ON THE STRUCTURE OF THE RHYNCHOLITES HADROCHEILUS (H.) OPTIVUS SHIMANSKY AND H. (H.)SSUM SHIMANSKY

dc.contributor.authorKomarov V.N.
dc.date.accessioned2021-02-24T07:52:24Z
dc.date.available2021-02-24T07:52:24Z
dc.date.issued2001
dc.description.abstractThe structure of the Lower Cretaceous rhyncholites H. (Hadrochelius) optivus and H. (H.)fissum is studied using SEM. Phyncholites are shown to consist of many alternating homogeneous layers of granular and cryptocrystalline calcite; each of these layers has an identical ultrastructure.
dc.identifierhttps://elibrary.ru/item.asp?id=13383319
dc.identifier.citationPaleontological Journal, 2001, 35, 5, 485-490
dc.identifier.issn0031-0301
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/25598
dc.subjectCretaceousen
dc.subject.ageMesozoic::Cretaceousen
dc.titleNEW DATA ON THE STRUCTURE OF THE RHYNCHOLITES HADROCHEILUS (H.) OPTIVUS SHIMANSKY AND H. (H.)SSUM SHIMANSKY
dc.typeСтатья

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