[b]The Jurassic succession of Ras Sharwayn, South-Eastern Yemen[/b]

Journal Title: Volumina Jurassica - Year 2009, Vol 7, Issue 1

Abstract

Four Jurassic stratigraphic units have been recognised at Ras Sharwayn, about 300 km east of Al-Mukalla along coast of the Gulf of Aden. The Kohlan Formation (60 m) unconformably overlies the crystalline basement. Its lower and middle part consist of fluviatile sandstone and conglomerate. The upper part is made up of transitional coarse- and fine-grained sandstones and siltstones. The sequence ends with shallow marine fine-grained sandstones. The Shuqra Formation (71 m) can be divided into two members. The lower Calcareous-marly Member (45 m) consists of grey bioclastic limestone andsubordinate nodular marl (inner to mid ramp). Its age is Late Oxfordian. The upper Carbonate Member (26 m) changes from basal reddish marly limestones (mid ramp) to thick beds of red-brown, coarsely crystalline limestones and dolomites (inner ramp). The topmost beds contain fossils of colonial organisms, essentially stromatoporoids. Its age is Late Oxfordian, and possibly earliest Kimmeridgian. The Madbi Formation (>30 m) consists of yellowish marl alternating with marly limestone and bioclastic limestone (coquinas) corresponding to storm layers (mid to outer ramp). With regard to its age, a specimen of [i]Orthosphinctes [/i]sp., collected a few metres from the base, possibly refers to the EarlyKimmeridgian. The Madbi Formation ends with an unconformity surface. The informal Clastic unit (56 m) (including the Naifa Formation) consists, from bottom upwards, of: red-brown dolomite; grey detrital limestone with quartz grains; massive, white conglomerate with well rounded limestone clasts, quartz and bioclasts (e.g. colonial organisms). The last lithotypes are gravity flow deposits, accumulated at the base of a scarp possibly tectonic in origin, approximately at the Jurassic-Cretaceous boundary.This detailed lithological, sedimentological and biostratigraphical study has provided revised lithostratigraphical subdivision and nomenclature and improved the stratigraphic control.

Authors and Affiliations

Milvio FAZZUOLI, Marco MORELLI, Giulio PAVIA, Khalid A. AL-THOUR, Maurizio CHIOCCHINI, Viviana REALE, Emma TADDEI

Keywords

Related Articles

[b]Ammonites from the Oxfordian-Kimmeridgian boundary and the Lower–Upper Kimmeridgian of Kachchh, western India[/b]

Several new specimens of ammonites from the Oxfordian and Kimmeridgian of Kachchh, western India, are described and illustrated. The Oxfordian ammonites ?[i]Subdiscosphinctes [/i]Malinowska, [i]Perisphinctes[/i] Waagen,...

Behavioural palaeobiology and taphonomy of the Late Jurassic calcareous sponge Elasmostoma fomes W. Müller, 1984

Calcareous sponges Elastostoma fomes W. Müller, 1984, from the Lower Kimmeridgian marly onkoliticlimestones exposed at Karsy in the Holy Cross Mountains, Central Poland, are studied in terms of their settlement, growth,...

Y GENERATION – A CHALLENGE FOR HUMAN RESOURCES DEPARTMENTS

This article attempts to answer the question what are the greatest challenges facing HR departments in connection with the phenomenon of generation Y, which was formed as a result of changes taking place in society, cult...

INTRAPERSONAL RELATIONS AS THE BASIS OF NON-PROFIT ORGANIZATIONS’ FUNDRAISING

The article presents the fundamentals of fundraising, as the key condition of the function-ing and development of non-profit organizations. Using this background, the importance of human capital and interpersonal relatio...

Download PDF file
  • EP ID EP67931
  • DOI 10.5604/17313708 .1139775
  • Views 55
  • Downloads 0

How To Cite

Milvio FAZZUOLI, Marco MORELLI, Giulio PAVIA, Khalid A. AL-THOUR, Maurizio CHIOCCHINI, Viviana REALE, Emma TADDEI (2009). [b]The Jurassic succession of Ras Sharwayn, South-Eastern Yemen[/b]. Volumina Jurassica, 7(1), 135-146. https://europub.co.uk/articles/-A-67931