Abstract This Passive margin in the Western Mediterranean formed by rifting of a back-arc basin during the Early-Mid Miocene, subsidence has led to the deposition of between two and ten kilometres of sediment of which 8 kilometres is believed to be prospective. It has two prospective petroleum systems, Pre-Messinian sourced chiefly in Oligocene Shales and Sapropels, these have not though been well explored and so there is a high degree of risk Exploring the licence area. The 2 nd is the Plio-Quaternary Upper Sequence, it is possible that some charge occurs from Pre-Messinia layers but without this charge may be accomplished by Biogenic processes releasing gas. The basin is a challenging exploration target as a result of salt, but with improved 3D and Multi-azimuth seismic and with other geophysical methods it should be possible to recognise the key geometries of the basin; rifts in the basement, prograding mud fans, the canyons and steeper, coarser grained fans of the Messinian Drawdown. In the upper sequence seismic resolution should be greatly improved and sands and mud drapes should be distinguishable. Immediate targets for exploration should be; undrilled Oligocene syn-rift sediment, drilling technology and funds allowing; and studies to understand structures/chaotic facies described in literature as possibe gas escape structures. Introduction The Rhone Maritime Area (RMA), offshore Southern France, lies in water depths of 2000 metres; a part of the submarine fan system originating on the Gulf of Lions platform it is a underlain by a 1
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Abstract
This Passive margin in the Western Mediterranean formed by rifting of a back-arc basin
during the Early-Mid Miocene, subsidence has led to the deposition of between two and
ten kilometres of sediment of which 8 kilometres is believed to be prospective. It has two
prospective petroleum systems, Pre-Messinian sourced chiefly in Oligocene Shales and
Sapropels, these have not though been well explored and so there is a high degree of risk
Exploring the licence area. The 2nd is the Plio-Quaternary Upper Sequence, it is possible
that some charge occurs from Pre-Messinia layers but without this charge may be
accomplished by Biogenic processes releasing gas. The basin is a challenging exploration
target as a result of salt, but with improved 3D and Multi-azimuth seismic and with other
geophysical methods it should be possible to recognise the key geometries of the basin;
rifts in the basement, prograding mud fans, the canyons and steeper, coarser grained fans
of the Messinian Drawdown. In the upper sequence seismic resolution should be greatly
improved and sands and mud drapes should be distinguishable.
Immediate targets for exploration should be; undrilled Oligocene syn-rift sediment, drilling
technology and funds allowing; and studies to understand structures/chaotic facies
described in literature as possibe gas escape structures.
Introduction
The Rhone Maritime Area (RMA), offshore Southern France, lies in water depths of 2000
metres; a part of the submarine fan system originating on the Gulf of Lions platform it is a
underlain by a passive margin formed by Oligocene rifting, oriented NE-SW, and Miocene
accretion of oceanic crust. Since the end of active Mid Ocean Ridge volcanism the RMA
and the wider Provence Basin have undergone considerable thermal subsidence.
Subsidence has resulted in continuous sedimentation along the margin with inflow from
the Alps, the Pyrenees & the Massive Central. The Gulf of Lyons shelf margin lies at ~90
kilometres from the coast, the shelf slope lies at ~160 km and salt diapirism can be
observed at between ~250 km to ~330 km from the coast of France at Agde (Google n.d.).
The Rhone Maritime Area is licensed by the French government to Melrose Resources
As no reserves are posted and no wells drilled it would be fair to use the USGS figure for
Resources, whilst qualifying it by saying that Pliocene-Quaternary Biogenic gas is
proposed which would add to reserves => 505 MMBOE {derived from Pawlewicz,
2004}. Melrose Resources have reported 10 Tcfe of reserves in their Rhone Maritime Area
License, it is hypothesised that these are the large fault bounded basement structures. As
yet it is not known when Melrose plan to drill these structures.
It is worthwhile examining the French government websites for information about the area,
where it is should be possible to access geographic information about the margin.
There is a very high degree of academic interest in the basin, and a large number of
publications relevant to the industry.
Conclusions
The Rhone Maritime Area is a good prospective basin, in a challenging environment and
would provide good opportunities for a farm-in. It might become a more strategically
important resource to the European Union if relations with Russia and the FSU worsen.
The most prospective reserves would be those in the Pre-Messinian sediments, it is
however the technical difficulties connected to exploiting these resources may make the
other less prospective resources more attainable. Particularly the resources Onshelf Gulf
of Lions, which lie on trend from the proven Camargue Basin. It would also be beneficial to
understand the wider petroleum system to drill through the Oligocene source section. The
targets are likely to be gravity and seismic anomalies, gravity data will prove particularly
useful to deal with the variations of acoustic properties through the Miocene evaporite
sequence.
Plio-Quaternary gas should be constrained with further geophysical/geochemical surveys
to investigate possible gas escape structures.
8
Acknowledgements
Dr Helen Lewis for reading lists.
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