RR,
I am in no way a professional chemist, mineralogist, or geologist -- just an old rockhound that has learned a lot from many folks much smarter than me and reading all I can about NC minerals. I will try to answer your questions as best I can. I'm sure Joe, Scott, John and others will chime in and correct me or add to what I have to offer.
Zeolites are microporous, hydrated aluminosilicate minerals. What makes them special is their ability to absorb water, and the water molecules are reflected in their chemical structure. Some examples of mineral zeolites are analcime, chabazite, clinoptilolite, heulandite, laumontite, natrolite, phillipsite, pollucite, scolecite, stilbite, and thomsonite. These are only a few of the many that have been described.
As you mentioned, zeolites were formed and occur in volcanic rocks and hydrothermal veins, and the best examples occur in basalt (India). Since real basalt is rare in NC where are these zeolites found? Igneous rocks (volcanic in origin) occur throughout the Piedmont and mountains in the form of andesites, diabases, diorites, granites (pegmatites), gneisses, rhyolite, and others. Although zeolites do not necassarily occur in all of these rocks, many of the large Martin-Marietta quarries in the Central Piedmont of NC are known for zeolites, such as stilbite, chabazite, and laumontite.
As far as I know, fluorescents do not form that close to zeolites in NC, other than calcite. Most fluorecents in NC are mainly calcite, hyalite opal, autunite (and other rare uranium minerals), corundum var. ruby, and fluorite. I'm sure there are others I'm forgetting. Most NJ fluorescents do not occur in NC, such as willemite and others known from the Franklin district.
I hope this was helpful.
Dennis
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