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2. Rare-earth mineral - Wikipedia

   en.wikipedia.org/wiki/Rare-earth_mineral

   Rare-earth mineral. Rare-earth ore, shown with a United States penny for size comparison. A rare-earth mineral contains one or more rare-earth elements as major metal constituents. Rare-earth minerals are usually found in association with alkaline to peralkaline igneous complexes in pegmatites. This would be associated with alkaline magmas or ...

3. Coupon - Wikipedia

   en.wikipedia.org/wiki/Coupon

   Coupon. In marketing, a coupon is a ticket or document that can be redeemed for a financial discount or rebate when purchasing a product. Customarily, coupons are issued by manufacturers of consumer packaged goods [1] or by retailers, to be used in retail stores as a part of sales promotions. They are often widely distributed through mail ...

4. Shortcuts.com has printable coupons - AOL

   www.aol.com/news/2010-05-04-shortcuts-com-has...

   To get printable coupons on Shortcuts.com, plug in your zip code. When I entered mine, 48 coupons popped up. If you are looking for more grocery coupons, check out Coupons.com , SmartSource , or ...

5. Baryte - Wikipedia

   en.wikipedia.org/wiki/Baryte

   Baryte, barite or barytes (/ ˈbæraɪt, ˈbɛər -/ BARR-eyet, BAIR-[7] or / bəˈraɪtiːz / bə-RYTE-eez[8]) is a mineral consisting of barium sulfate (Ba S O 4). [3] Baryte is generally white or colorless, and is the main source of the element barium. The baryte group consists of baryte, celestine (strontium sulfate), anglesite (lead ...

6. AOL Mail

   mail.aol.com

   Get AOL Mail for FREE! Manage your email like never before with travel, photo & document views. Personalize your inbox with themes & tabs. You've Got Mail!

7. Polymetallic replacement deposit - Wikipedia

   en.wikipedia.org/wiki/Polymetallic_replacement...

   Cartoon cross-section showing manto ore deposits (USGS) [1] A polymetallic replacement deposit, also known as carbonate replacement deposit or high-temperature carbonate-hosted Ag-Pb-Zn deposit, [2] is an orebody of metallic minerals formed by the replacement of sedimentary, usually carbonate rock, by metal-bearing solutions in the vicinity of igneous intrusions. [3]