
10–11March 2008
Abdallah Ait Salem, ONHYM; Mostafa Amrhar, Marrakech University; and Hassan Tourani, Marrakech University
USD 350
Limit: Minimum 15 persons; maximum 30 persons
Registration deadline: 28 February 2008
This field trip is ideal for anyone wishing to see and examine the superb Triassic outcrops of Morocco — world-class geological structures that resulted from inverted early rifting deposits of Triassic red beds, and spectacular scenery on the High Atlas chain culminating at more than 3,000 m above the Marrakech plain.
Plan to explore what could be theTriassic outcrop analogues of the reservoir rocks in the Meskala gas and condensate field and the Trias Argileux Greseux Inferieur (TAGI) in Algeria. The main sections of outcrops are located in the Argana valley, which has an Atlantic obedience, and the Ourika valley, which is believed to belong to the Thetys seaway; both sections consist of continental red beds, grading upwards from alluvial conglomerates into fluvial and Aeolian sandstone and shale, and finally into sebkha-type salt.
The basal sediments have filled tectonically subsiding grabens and/or half grabens while the upper deposits spread out over larger areas and cover the uplifted blocks.
The reservoir quality of the sandstones varies vertically and laterally depending on their respective depositional environments and settings.
Looking across the most beautiful valleys of the Atlas Mountains, you will discover small hamlets on the cliff side and a potters’ village on the bank of the fresh waters of the Ourika and Argana valleys. Enjoy lunch in the heart of the mountains in a traditional Berber dwelling while taking in the magnificent panoramic view.
Departure: Marrakech to Oukaimiden
The Oukaimeden Triassic section crops out 60 km southwest of Marrakech,
along the Ourika valley (Oued Ourika) in the central High Atlas, known also as
Atlas of Marrakech.
From the Aghbalou village to the Oukaimiden village, the outcropping section comprises a succession from Permian to Upper Triassic and exhibits an outstanding exposure of the uppermost F-4, F-5, and F-6 members of the Oukaimiden formation.
Stop 1-1: Oukaimiden Lake
See the top F-5 member with fluvial and aeolian sediments.
Stop 1-2: East of Okaimiden Village
Identify different members of the Oukaimiden formation, and understand
their vertical and lateral variations across the basin.
Lunch
Stop 1-3: Andrar-n-Tizrag
See the contact with the basement, the lower and middle members of the
formation, as well as the gradual change from F-4 to F-5 members.
Stop 1-4: Agsarane
Appreciate the effects of Atlas inversion (alpine) at one of the North
Atlasic Thrust faults.
Stop 1-5: Fum Lgha
See local changes in lithology of the F-5 member close to the
hinterland.
Return to Marrakech
Departure from Marrakech to Argana
Because it belongs to the Moroccan Atlantic margin and its location is
adjacent to the Essaouira basin, the Argana valley is commonly identified as
the most appropriate outcrop analogue of the subcropping Triassic sub-basins
infill succession.
The T-6 member of the Argana formation, particularly, provides key information for understanding the three-dimensional distribution as well as the modelling of the reservoir.
The stops are located along the main road, Marrakech-Agadir, and allow a better understanding of the reservoir distribution in the basin.
Stop 2-1: Amzri
This outcrop shows the internal organization of the sand bodies within the
T-6 member and consequently helps in the interpretation of depositional
environment.
Stop 2-2: Argana village
This outcrop is the best illustration of the relationship between the main
reservoir member (T-6) and the bounding members (T-5 and T-7).
Lunch
Stop 2-3
The T-6 member becomes thicker at this location.
Return to Marrakech