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Minette-type iron deposits are a specific kind of oolitic iron deposit formed in shallow, near-shore marine environments. These deposits are characterized by small, rounded masses called ooliths, which are composed of iron minerals such as siderite, chamosite, and goethite. Historically, these deposits were a significant source for the iron and steel industries in Europe and North America. They are most extensively developed in areas like England, the Lorraine region of France, Belgium, and Luxembourg. Minette-type deposits are distinguished from similar Clinton-type deposits found in North America by the presence of goethite.1

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