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 .
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| - تشكيل هرمز الجيولوجي (ar)
- Hormuz Formation (en)
- Formazione di Hormuz (it)
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| - 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)
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| - 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)
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