Letters to the Editor

History and the Oman Mountains

Regarding your article “Medalist a World Geologist” (June EXPLORER), on the occasion of Ken Glennie’s well-deserved award of the Sidney Powers Medal:

I was a colleague of Ken during my career as an explorationist with the Royal Dutch-Shell Group. In fact, upon completion of my basic training with the company in late 1963, my first overseas assignment was supposed to be a six months “roving party” with Ken in Afghanistan. Plans changed, however, and in January 1964 I was sent to Oman instead, first as well-site geologist for six months then as field geologist for two years. This was just before Ken would move his studies of recent desert sedimentation to Oman.

Regarding the structural interpretation of the Oman Mountains, Glennie is quoted as saying: “I led a team mapping the Oman Mountains. In all the work previous to that, everyone had thought that all the rocks were deposited where they currently were found.”

Actually, sedimentary rocks of the Hawasina Group and basic/ultra-basic rocks of the Semail Group were first recognized in 1904-05 by Pilgrim, but it was in 1928 that Lees, an IPC geologist, published the results of his and Gray’s memorable geological survey of the interior of the Oman Mountains. With profound insight, Lees concluded that both the Hawasina and the Semail had been emplaced as huge nappes thrusted during the Upper Cretaceous.

After World War II, IPC was exploring the Oman petroleum concession and their geologists carried out more extensive fieldwork from 1949-60, the results of which are mostly in unpublished reports. During that period a drastic change of ideas was introduced by Morton, who made the Hawasina a lateral equivalent of the clearly autochthonous Aruma shales found in the desert wells, and abandoned the concept of thrust sheets altogether.

Following the drilling by IPC of a number of unsuccessful exploration wells, their Oman concession was taken over, lock, stock and barrel, by Shell.

The first Shell fieldwork campaign (1963-64) was carried out by Hans Kapp and Peter Llewellyn, who made a comprehensive survey of the autochthonous sediments of the central Oman Mountains. With respect to the Hawasina and Semail, a secondary objective, they stuck to Morton’s ideas.

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History and the Oman Mountains

Regarding your article “Medalist a World Geologist” (June EXPLORER), on the occasion of Ken Glennie’s well-deserved award of the Sidney Powers Medal:

I was a colleague of Ken during my career as an explorationist with the Royal Dutch-Shell Group. In fact, upon completion of my basic training with the company in late 1963, my first overseas assignment was supposed to be a six months “roving party” with Ken in Afghanistan. Plans changed, however, and in January 1964 I was sent to Oman instead, first as well-site geologist for six months then as field geologist for two years. This was just before Ken would move his studies of recent desert sedimentation to Oman.

Regarding the structural interpretation of the Oman Mountains, Glennie is quoted as saying: “I led a team mapping the Oman Mountains. In all the work previous to that, everyone had thought that all the rocks were deposited where they currently were found.”

Actually, sedimentary rocks of the Hawasina Group and basic/ultra-basic rocks of the Semail Group were first recognized in 1904-05 by Pilgrim, but it was in 1928 that Lees, an IPC geologist, published the results of his and Gray’s memorable geological survey of the interior of the Oman Mountains. With profound insight, Lees concluded that both the Hawasina and the Semail had been emplaced as huge nappes thrusted during the Upper Cretaceous.

After World War II, IPC was exploring the Oman petroleum concession and their geologists carried out more extensive fieldwork from 1949-60, the results of which are mostly in unpublished reports. During that period a drastic change of ideas was introduced by Morton, who made the Hawasina a lateral equivalent of the clearly autochthonous Aruma shales found in the desert wells, and abandoned the concept of thrust sheets altogether.

Following the drilling by IPC of a number of unsuccessful exploration wells, their Oman concession was taken over, lock, stock and barrel, by Shell.

The first Shell fieldwork campaign (1963-64) was carried out by Hans Kapp and Peter Llewellyn, who made a comprehensive survey of the autochthonous sediments of the central Oman Mountains. With respect to the Hawasina and Semail, a secondary objective, they stuck to Morton’s ideas.

Party chief Peter Kassler and I did the second Shell campaign (1964-65). Part of it dealt with the Haushi-Huqf area in southern Oman, the other part was devoted to “plugging the holes” and extending the surveyed area of the previous campaign. That is when Kassler and I started to express some doubts as to the validity of Morton’s ideas, following

our field observations in the Hawasina and Semail rocks.

For the third Shell field season (1965- 66), I was party chief and my co-worker was Jan Horstink. On our request, our bosses agreed that the campaign would be devoted to the unraveling of the Hawasina-Semail complex. As work progressed, we could subdivide the Hawasina and map its various units (a number of the current formation names are ours) and observe its relationships with the overlying Semail and underlying sediments. It became more and more evident that we were in the presence of huge allochthons, just as Lees had thought 40 years before.

The Shell field seasons lasted from early October to May, seven days a week under the tent or the stars, with a two-week leave over Christmas and New Year – truly the good old days! Thus, much mapping had been carried out in the Oman Mountains before Glennie’s arrival.

Another of Glennie’s quotes was: “The reason for going back to Oman was that the head of Shell’s global exploration had been on a field trip to Oman in the 1960.”

Indeed, this visit by Rudi Beck took place during my second field season. I took him around for a couple of days, showing him why we favored an allochthonous origin for the Hawasina and the Semail. At the same time, I told him that this type of fieldwork was not very relevant to petroleum exploration and would best be carried out by university people who had the time that we did not have. He then said, at the foot of an exotic block in the Wadi Hawasina, that it could be a job for the Shell exploration lab people, “as they have spent enough time already on delta and desert studies.” At the moment, I did not give much importance to this statement.

Unknown to us, of course, was the fact that our re-interpretation of the Oman Mountains structure gave rise to much controversy in the Oman and Hague offices, where Morton’s ideas were taken for granted.

In 1966, when Horstink and I were back in the Netherlands at the research lab to write our report, we were surprised to learn that an Oman Mountains team was being formed there, comprising Michel Boeuf, Mike Hughes-Clarke, Mark Moody-Stuart (future Shell CEO), Pete

Pilaar and Ben Reinhardt, under the leadership of Ken Glennie.

Our report (unpublished), “The Mesozoic Nappes of the Oman Mountains” was completed in January 1967. In 1973 the Glennie group published the article “Late Cretaceous Nappes in the Oman Mountains and Their Significance” in the AAPG BULLETIN. In 1974 the book “Geology of the Oman Mountains” was published. In its early pages, a couple of lines refer to Jan Horstink’s and my interpretation.

As far as the prospectivity of the sub- Hawasina structures was concerned, a well was drilled later on one of the four possible locations selected by Horstink and myself. The results showed that the Oman Mountains acreage could be safely relinquished.

I have kept imperishable memories of my time in Oman, certainly the best of my Shell career. Still, in retrospect, I regret that Jan Horstink and I did not publish a paper in 1967. However, I had just gotten married, was on my way to Canada and Horstink was back in Oman as field party chief.

I think that the “inside story” of Oman Mountains’ successive interpretations could be of interest to the readers of the EXPLORER, especially the younger ones, as the days of large scale, exciting and ground-breaking field work by oil geologists in more or less unknown areas is over.

And, a word of advice to them: Publish early if you have something really new to say!

Jean Haremboure,
Allan, France


Drill It

I am greatly disappointed in the trend toward questionable science and zealotry expressed in letters to the EXPLORER.

Creationism and God belong in churches, not in AAPG journals. Instead we should be seeing discussions on how

to best educate the public on evolution, to prevent blunders like the Kansas board of education. If the body of AAPG members cannot resolve nonsense like intelligent design/creationism and the difference between faith (believing without evidence or data) and theory (rigorous testing of ideas against

observed data), then this organization is in serious trouble.

Like evolution, the data for global warming is overwhelming. If this data were a prospect, we would have drilled it years ago.

David Gallaher.
Idaho Springs, Colo.

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