About: Hormuz Formation     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : owl:Thing, within Data Space : dbpedia.demo.openlinksw.com associated with source document(s)
QRcode icon
http://dbpedia.demo.openlinksw.com/c/4UZYkNj3NK

The Hormuz Formation, Hormuz Series, Hormuz Evaporites or Hormuz Group is a sequence of evaporites that were deposited during the Ediacaran (Late Neoproterozoic) to Early Cambrian, a period previously referred to as the Infra-Cambrian. Most exposures of this sequence are in the form of emergent salt diapirs within anticlines of the Zagros fold and thrust belt. As a result of their involvement in post-depositional salt tectonics, the internal stratigraphy of the sequence is relatively poorly understood. They are the lateral equivalent of the evaporite-bearing Ara Group in the .

AttributesValues
rdfs:label
  • تشكيل هرمز الجيولوجي (ar)
  • Hormuz Formation (en)
  • Formazione di Hormuz (it)
rdfs:comment
  • تشكيل هرمز أو سلسلة هرمز أو متبخرات هرمز أو مجموعة هرمز هو سلسلة من المتبخرات التي تم إيداعها خلال العصر الإدياكاري (أواخر حقبة الطلائع الحديثة) في العصر الكامبري المبكر، وهي الفترة التي يشار إليها سابقا باسم تحت-الكامبري. يظهر هذا التشكيل في معظم الحالات في شكل قباب ملحية ناشئة ضمن الطيات المحدبة. تسلسل الطبقات الداخلية غير مفهوم نسبيًا نتيجة لتداخلها في ‏ بعد الترسيب. وهي المكافئ الجانبي لمجموعة آرا المتبخرة في حوض جنوب عمان. (ar)
  • The Hormuz Formation, Hormuz Series, Hormuz Evaporites or Hormuz Group is a sequence of evaporites that were deposited during the Ediacaran (Late Neoproterozoic) to Early Cambrian, a period previously referred to as the Infra-Cambrian. Most exposures of this sequence are in the form of emergent salt diapirs within anticlines of the Zagros fold and thrust belt. As a result of their involvement in post-depositional salt tectonics, the internal stratigraphy of the sequence is relatively poorly understood. They are the lateral equivalent of the evaporite-bearing Ara Group in the . (en)
  • La formazione di Hormuz, conosciuta anche come serie di Hormuz, evaporiti di Hormuz e gruppo di Hormuz, è una sequenza di evaporiti depositatesi dall'Ediacarano, il terzo e ultimo periodo geologico dell'era Neoproterozoica, fino al Cambriano inferiore, un periodo che, in letteratura, viene talvolta chiamato Infra-Cambriano. La maggior parte delle evidenze di questa sequenza di strati è rappresentata da diapiri salini che affiorano in superficie dall'interno degli anticlinali della cintura di piegatura e spinta degli Zagros, in particolare nella sua regione sud-orientale. (it)
foaf:depiction
  • http://commons.wikimedia.org/wiki/Special:FilePath/SaltGlaciers_ZagrosMtns_20010810.jpg
dct:subject
Wikipage page ID
Wikipage revision ID
Link from a Wikipage to another Wikipage
sameAs
dbp:wikiPageUsesTemplate
thumbnail
has abstract
  • تشكيل هرمز أو سلسلة هرمز أو متبخرات هرمز أو مجموعة هرمز هو سلسلة من المتبخرات التي تم إيداعها خلال العصر الإدياكاري (أواخر حقبة الطلائع الحديثة) في العصر الكامبري المبكر، وهي الفترة التي يشار إليها سابقا باسم تحت-الكامبري. يظهر هذا التشكيل في معظم الحالات في شكل قباب ملحية ناشئة ضمن الطيات المحدبة. تسلسل الطبقات الداخلية غير مفهوم نسبيًا نتيجة لتداخلها في ‏ بعد الترسيب. وهي المكافئ الجانبي لمجموعة آرا المتبخرة في حوض جنوب عمان. (ar)
  • The Hormuz Formation, Hormuz Series, Hormuz Evaporites or Hormuz Group is a sequence of evaporites that were deposited during the Ediacaran (Late Neoproterozoic) to Early Cambrian, a period previously referred to as the Infra-Cambrian. Most exposures of this sequence are in the form of emergent salt diapirs within anticlines of the Zagros fold and thrust belt. As a result of their involvement in post-depositional salt tectonics, the internal stratigraphy of the sequence is relatively poorly understood. They are the lateral equivalent of the evaporite-bearing Ara Group in the . (en)
  • La formazione di Hormuz, conosciuta anche come serie di Hormuz, evaporiti di Hormuz e gruppo di Hormuz, è una sequenza di evaporiti depositatesi dall'Ediacarano, il terzo e ultimo periodo geologico dell'era Neoproterozoica, fino al Cambriano inferiore, un periodo che, in letteratura, viene talvolta chiamato Infra-Cambriano. La maggior parte delle evidenze di questa sequenza di strati è rappresentata da diapiri salini che affiorano in superficie dall'interno degli anticlinali della cintura di piegatura e spinta degli Zagros, in particolare nella sua regione sud-orientale. Dato il coinvolgimento della sequenza degli strati nella tettonica salina che ha seguito la loro deposizione, la stratigrafia interna della formazione di Hormuz è piuttosto complessa e ancora non del tutto chiara anche se in gran parte compresa. Tali strati sono considerati l'equivalente laterale del gruppo dell'Ara, nel meridionale. (it)
prov:wasDerivedFrom
page length (characters) of wiki page
foaf:isPrimaryTopicOf
is Link from a Wikipage to another Wikipage of
is Wikipage disambiguates of
is foaf:primaryTopic of
Faceted Search & Find service v1.17_git147 as of Sep 06 2024


Alternative Linked Data Documents: ODE     Content Formats:   [cxml] [csv]     RDF   [text] [turtle] [ld+json] [rdf+json] [rdf+xml]     ODATA   [atom+xml] [odata+json]     Microdata   [microdata+json] [html]    About   
This material is Open Knowledge   W3C Semantic Web Technology [RDF Data] Valid XHTML + RDFa
OpenLink Virtuoso version 08.03.3331 as of Sep 2 2024, on Linux (x86_64-generic-linux-glibc212), Single-Server Edition (378 GB total memory, 59 GB memory in use)
Data on this page belongs to its respective rights holders.
Virtuoso Faceted Browser Copyright © 2009-2024 OpenLink Software