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Lithostratigraphy of Iran

Part of the Springer Geology Book Series

DOI: 10.1007/978-3-030-04963-8

ISBN: 978-3-030-04962-1

Publisher: Springer International Publishing - Springer Journals

Jan 18, 2019

Available

Precambrian

Ghorbani, Mansour

Pages: 1 –23

[Being the longest Eon, the Precambrian is divided into the Archean and the Proterozoic which are further divisible into smaller units (Fig. 1.1).]
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Paleozoic

Ghorbani, Mansour

Pages: 25 –130

[Being the longest Phanerozoic eras, the Paleozoic is a most geologically important era in the geology of Iran.]
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Mesozoic

Ghorbani, Mansour

Pages: 131 –223

[The Mesozoic era consists of three periods the Triassic, Jurassic and Cretaceous spanning in total 186 Myr (Fig. 3.1). ]
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Cenozoic

Ghorbani, Mansour

Pages: 225 –263

[The Cenozoic Era begins at 65 Ma and continues to the present day (Fig. 4.1). At the beginning of this era, the earth was experiencing some tectonically-important evolutionary events that affected the geological and stratigraphical history of Iran. These results will be discussed below. ]
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Plio-Quaternary

Ghorbani, Mansour

Pages: 265 –276

[The upper Pliocene rocks in Iran cannot be distinguished from those of lower Quaternary owing to the same dominant environment conditions. In this context, some geological events started from the late Pliocene and continued through the early Quaternary such as sedimentation of Hezardarreh...

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