Saturday, September 9, 2017

#somepapers No. 8: The biggest gold mine in Canada*

The Paper

Mercier-Langevin, P., Dube, B., Hannington, M.D., Davis, D.W., Lafrance, B., and Gosselin, G, 2007, The LaRonde Penna Au-rich volcanogenic massive sulfide deposit, Abitibi Greenstone belt, Quebec: Part I. Geology and geochronology. Economic Geology, v. 102, p. 585-609.


What it says

The LaRonde deposit is a very large gold deposit in the Abitibi Greenstone belt which, at the time this paper was written, was the largest gold mine in Canada. It had production and reserves of 8.1 Moz of gold, with a whole mess of base metals and silver in there, too. This mine is still going strong, with 5.6 Moz Au still in the ground (reserves plus resources). This paper is the first of three that covers the geology, geochemistry, and alteration of this important deposit in the far eastern Abitibi.

This paper is mostly descriptive, reporting on the volcanic sequence that hosts the Au deposit. The volcanic package spans a range of compositions, from basaltic andesite through rhyolite. In contrast to some other deposits in the region, the host rocks of LaRonde were not a bimodal. The composition evolved throughout the couple of million years these rock were erupted and emplaced.

The authors also presented new U-Pb dates for the hanging wall and footwall of the 20 North ore lens, which was the active orebody at the time this paper was written. They showed a pretty tight window for the formation of the massive sulfide deposit around 2698 Ma. These new dates bracket the VMS mineralization. Because the LaRonde deposit is much less deformed than some of the other large Au-rich VMS deposits in the Abitibi, the timing relationships between Au and base metals is more clear; the gold at LaRonde was introduced syngenetically, rather than being introduced during later deformation.

Even though LaRonde is less deformed than some other deposits, from my point of view as a geologist who's spent most of his time in the Great Basin, these Archean greenstones are pretty beat up.

Why it matters

This is an important type of Canadian gold deposit. Understanding the kinds of rocks where they form helps us find more. Linking the Au mineralization to the VMS deposition, and not to a later structural event, also helps geologists understand their deposit and reduce the risks of discovery and mining.

Why I read it

Last month I spent a week up in the Abitibi for work. The company I work for, Agnico Eagle owns LaRonde, and it's one of our major producers. The the corporate technical services group works out of a mine building near the property and I was heading up there for some training.

While I was up there, I realized I really didn't know anything about the geology under my feet. I did know I was in the Abitibi Greenstone belt, home to "Archean gold deposits" as I learned in my Economic Geology course. I didn't know much more about the gold in this part of the world. I sought out some paper, any paper, really, about the deposit I was driving to every day that week. This is the one I found. Pretty good one. Might have to check out the rest of the series.

Odds and Ends

Heading up to this part of Quebec was an interesting experience. I've visited a handful of countries in my life, but I'm not really what you'd consider a "traveler". Before this trip I had been to Chile a couple times for field courses, Italy for a conference, and Vancouver to visit UBC. I stayed in Val-d'Or, a nice, if small town a few hours from Montreal. Turns out, this part of Quebec (and maybe the rest of it, too) is very French. I was not expecting that, but I got by.

My last night there, I took the recommendation of one of the geologists in the modeling group and went to l'Entracte. It was Friday and packed. I had no reservation, so I took a seat at the bar and ordered a Coke (as a teetotaler, this isn't usually my preferred seat). people around me were talking, and generally having a good time. Except for one pair of guys at the other end of the bar talking mining, or maybe geology, everyone was having a good time in French.

I ordered the salmon and asparagus, easily the best meal I had that week. Soon an older, thin gentlemen sat down on my left and ordered a beer. When he paid, his brightly colored plastic money jumped from his hands and landed in "my" space. He said something in French, a joke I think, assuming we had a shared language. I nodded and smiled but understood nothing. Went back to my dinner.

The man stood and went to talk to the manager, or maybe owner, of the restaurant, used the phone. When he came back and sat down, he struck up a conversation in halting, heavily accented English. He introduced himself as Jean-Paul. He was waiting for his wife, who was coming to meet him for dinner. He asked where I was from and what brought me to the Abitibi. He was born in the town 78 years ago, in 1939 and had deep roots in the place. His brother owns the movie theater next door. Jean Paul has lived in Val-d'Or his entire life. After telling me this he paused and said, "And I am going to die here."

I was unsure whether he was just proud of his home or if there was something more certain in his proclamation. He explained that he had just been to the doctor that afternoon and had been diagnosed with pancreatic cancer. He had about six months to live. Besides his family, I was the second person he had told this, the first being the manager of the restaurant when he went to use the phone.

He told me about his diagnosis and his outlook. There was some tension in his face, maybe some fear, but mostly he seemed content. Not resigned. Not angry. This man who was just told he had six months to live, who had just learned he wouldn't see his 80th birthday was smiling and laughing, talking about his children and grandchildren and waiting for his wife. He apologized for his English one more time, and his wife arrived at the same time as the check for my dinner. I paid, and waited awkwardly for a pause in his conversation to tell him what a pleasure it was to meet him. Then I left, alone, as he was talking and laughing with his wife and another friend from town.

This short conversation at a bar on the east end of a little mining town in Quebec is still with me and still fills me with a certain wonder. During that short conversation I felt a bond with this stranger that was as strong as I feel with friends and acquaintances I've known for years. In that short time on a cool Friday night. I have very little in common with Jean-Paul. We are from different countries, speak different languages (for the most part), and have lived different lives. The only thing we really shared was our humanity.

It was a special experience, a singular feeling, bordering on sacred. It made the world feel small and connected.

I don't think I have the words to do justice to how that experience made me feel. I think it's why people travel. Not just visit a resort here and there, or go on a cruise, but really get out there and travel. It makes the world smaller and drives home the point that we really are in this together.











Wednesday, September 6, 2017

The World of Ideas

Last night I went to the monthly meeting fo the Arizona Geological Society. The talk was about the Enlightenment and how it helped kick off geology as it's own branch of science. Something like that, anyway. The speaker, Vic Baker or the University of Arizona, is an engaging speaker, and that surely helped draw me in. But what really grabbed me was the deeper, more romantic notion of ideas and their evolution over the 18th and 19th centuries. I came out of it with a book recommendation (The Invention of Nature by Andrea Wulf) and a desire to abandon Twitter and as the kids say, read all the things.

It was the first time in a few years that I've been to a geology talk like this, a talk where somebody gets up and speaks for an hour about a series of disparate ideas that come together to make a larger story. I realized last night how much I have missed that.

For most of the past twenty years I wanted to teach. That was a driving force behind my sticking with my PhD program, despite struggling through writing while working full time through the last five years of it. I wanted to get a tenure-track job working at a school with an MS program, and maybe a bit more of a teaching load than most people like.

This struck me as the best way to keep myself surrounded by ideas, and the idea of ideas, if that makes sense. I always found teaching the most rewarding part of my many years as a graduate student. It was always a pleasure helping others find their way through difficult subjects (and the not so difficult ones, too). When I wasn't teaching, I'd be expanding humanity's understanding of some esoteric bit of the earth. Judging from what I see on Twitter, most of the hard work of pushing the boundaries of science consists of writing proposals. Still, it sounded like a good deal.

The academic track didn't work out for me, so I spend most of my time in the world of production and results, pushing the bounds of block models and drill results. It's fulfilling work, but it isn't my passion. It isn't reading and thinking and writing, generating raw ideas, floating in the ether.

That's what this blog is about. It's encouragement to have new ideas in the of geology and revisit old ones. It's an opportunity for me to take trips into the world of ideas and spend a bit more time there, writing up a short report about what I found. I don't get to spend my life getting lost on the side roads in this world. But I'm glad I get a chance to visit and bring you along.

Sunday, September 3, 2017

#somepapers No. 7: An unusual epithermal system in Colombia

The paper

Rodriguez Madrid, A.L., Bissig, T., Hart, C.J.R., and Mantilla Figueroa, L.C., 2017, Late Pliocene high-sulfidation epithermal gold mineralization at the La Bodega and La Mascota deposits, northeastern Cordillera of Colombia. Economic Geology, v. 112, p. 347-374.

What it says

This paper is a pretty good example of a fairly common type of Master's thesis in economic geology. the authors describe the local geology, alteration, and mineralization stages and add some fluid inclusion and stable isotope work, for good measure. This sort of study is very useful to geologists like me who are working on a deposit and need to get up to speed on what is generally going on, but don't have the time to spend a summer figuring it out.

The La Bodega and La Mascota high sulfidation epithermal Au deposits are located in the Maricaibo tectonic block in northern Colombia. They are unusual because they are located more than 500 km from the nearest subduction zone. This type of deposit is generally coeval with shallow intrusions and volcanic rocks in volcanic arcs. There are Miocene (~10 Ma) porphyries in the district that did lead to some porphyry-style mineralization. However, Ar-Ar dates reported in this paper Au-Ag show the main stages of mineralization (there were 6 hydrothermal events here) are much younger, around 2 Ma. The highest grades are found in silicified breccias, which is pretty typical. Very little vuggy quartz has been found in this deposit, which is not so typical for this type of deposit (high sulfidation epithermal).

Why it matters

I don't know enough about epithermal deposits to say whether there's anything groundbreaking in these results, though I suppose high sulfidation deposits away from the volcanic arc is something new to think about.

These types of "typical" deposit work-ups are important to read because they help build geologists up a catalog of deposits to know what's normal. All deposits are different, but there's a lot of overlap. Understanding what parts of a deposit are normal and what are outliers can reduce the risks involved in drilling and mining. My job as a geologist in mining and exploration is to reduce risk; having a solid understanding of the deposit is key in reducing risk.

Why I read it

Epithermal deposits have become much more important to me than then were a couple months ago because I have a new job where we're looking for and mining these kinds of deposits. Although we don't have any mines or projects in this district, it's a good write up. It add to my my epithermal database. Another reason I read this paper is that this issue or Economic Geology was available, not packed up with all my office stuff.

Odds and Ends

One unusual aspect of this deposit is that the last stage of mineralization contained Zinc and Uranium. I was expecting some sphalerite, after all, it's hard to have a magmatic-hydrothermal deposit without some Zn floating around. But pitchblende?! Weird.

This is just the kind of thing that makes me happy to read a lot of papers and build my database. I'm still working on reading "a lot" of papers, but I'll get there.