ࡱ> ji u'\pSusanKehm Ba==X>(8X@"1Arial1Arial1Arial1Arial1Arial1Arial1Arial"$"#,##0_);\("$"#,##0\)!"$"#,##0_);[Red]\("$"#,##0\)""$"#,##0.00_);\("$"#,##0.00\)'""$"#,##0.00_);[Red]\("$"#,##0.00\)7*2_("$"* #,##0_);_("$"* \(#,##0\);_("$"* "-"_);_(@_).))_(* #,##0_);_(* \(#,##0\);_(* "-"_);_(@_)?,:_("$"* #,##0.00_);_("$"* \(#,##0.00\);_("$"* "-"??_);_(@_)6+1_(* #,##0.00_);_(* \(#,##0.00\);_(* "-"??_);_(@_)                + ) , *  (   (    (  `cXREADMEYSheet1T IdCountAcres/red and grey clay, kaolin, silica sand, lignite undividedllacustrine limestone, siltstone, chert, fluvial sandstone, >40 m (Hettangian and younger vertebrate fossils)fluvial, deltaic, lacustrine, playa and aeolian clastic rocks, lacustrine limestone and basalt agglomerate, >200 m (Hettangian and younger vertebrate fossils and spores)]tholeiitic plateau basalt, 270 m (U-Pb concordant zircon age in basal flow of 202+/-1 Ma(25)) tholeiitic plateau basalt, 100 mlacustrine playa, sandflat, and deltaic clastic rocks, minor aeolian sandstone and conglomerate, 200 m (?Carnian-Hettangian spores and fossils)lacustrine playa, sandflat, and deltaic clastic rocks, minor aeolian sandstone and conglomerate, 10-180 m (?Carnian-Hettangian spores and fossils)fluvial sandstone and conglomerate, aeolian sandstone, minor deltaic-lacustrine deposits, >300 m (Anisian-?Carnian spores and fossils)fluvial sandstone and conglomerate, aeolian sandstone, minor deltaic-lacustrine deposits, 0-300 m (Anisian-?Carnian spores and fossils)floodplain mudstone, fluvial sandstone, arkosic sandstone, minor conglomerate and lacustrine limestone, 350->400 m (Stephanian spores)nfloodplain mudstone, fluvial sandstone, conglomerate, rare lacustrine limestone, 300-350 m (Stephanian spores)fluvial sandstone, conglomerate, floodplain mudstone, mudstone, rare lacustrine limestone, 800-900 m (Westphalian D-Stephanian spores) Paraconformable to unconformable on most Carboniferous-Devonian unitsQfluvial sandstone, minor conglomerate, >200 m (Westphalian D - Stephanian spores)}fluvial and lacustrine mudstone, shale, siltstone, sandstone, limestone, coal, 700-1000 m (Westphalian C - Stephanian spores)Pfluvial sandstone, siltstone, shale, minor coal, >250 m (Westphalian C-D spores)Tfluvial conglomerate, sandstone, siltstone, mudstone, 600 m (Westphalian B-C spores)\fluvial siltstone, mudstone, sandstone, calcrete, minor coal, 0-200 m (Westphalian C spores)fluvial sandstone, minor conglomerate, mudstone and coal, 700 m (Westphalian B-C spores)Unconformable on Mabou and Windsor Groupsfluvial sandstone, conglomerate, coal and shale, 800-1000 m (Westphalian C and Stephanian spores)Unconformable on Windsor and Horton Groups, and Proterozoic-Paleozoic units in Mabou Highlandsfluvial-lacustrine sandstone, shale, siltstone, coal, limestone, >1900-2700 m (Westphalian A spores) Conformable-unconformable on Pomquet and Hastings Formationsfluvial sandstone, siltstone, mudstone, rare coal, 700 m (Westphalian A spores)Unconformable on Mabou Group, Devonian volcanic rocks, Cambro-Ordovician and Proterozoic rocks}fluvial sandstone, siltstone, shale, >400 m (Early Westphalian plants and spores)Unconformable on Visean-Namurian Mabou Group|lacustrine-alluvial shale, sandstone, minor conglomerate, oil shale, coal (early Westphalian C - early Westphalian D spores)4alluvial conglomerate, minor sandstone and siltstonejBraided stream sandstone, mudstone, rare coal and lacustrine limestone, 100-400 m (Westphalian C-D spores)pfluvial sandstone, conglomerate, mudstone, rare coal and lacustrine limestone, 0-1000 m (Westphalian B-C spores)*see individual listings for LCCm and LCCrrXfluvial sandstone, mudstone, local lacustrine limestone, 0-1000 m (Westphalian B spores)zfloodplain mudstone, minor sandstone, coal, lacustrine limestone and shale, 0-1450 m (Westphalian A-B spores and bivalves)alluvial conglomerate, sandstone, rare mudstone, 0-1500 m (Westphalian A-B spores)Conformable to unconformable on Boss Point Formation`fluvial sandstone, calcrete limestone, conglomerate, mudstone, 200-1200 m (Westphalian A spores)Nalluvial conglomerate and sandstone, 50-1500 m (Namurian-Westphalian A spores)Fundivided Conformable to unconformable on Devonian Fountain Lake Group^siltstone, minor sandstone, gypsum and anhydrite, >150 m (Visean (Brigantian)-Namurian spores)kfloodplain mudstone, fluvial sandstone, rare conglomerate and limestone, 200-750 m (Asbian-Namurian spores)1fluvial siltstone and sandstone (Namurian spores)Mfluvial shale, siltstone, minor lacustrine limestone (Asbian-Namurian spores)ffluvial siltstone, sandstone, minor conglomerate and lacustrine limestone, 100-500 m (Namurian spores)lacustrine-marine shale, siltstone, stromatolitic limestone, gypsum and anhydrite, 100-300 m (Brigantian-Namurian spores) Conformable-disconformable on Windsor Groupundivided, 1000 mesiltstone, minor gypsum and shallow marine limestone (Visean (Asbian), C-E subzones fauna and spores)hgypsum, minor siltstone, marine limestone and dolostone (Visean (Holkerian), B subzone fauna and spores)anhydrite, salt, marine dolostone and limestone (Visean (Arundian), A subzone fauna and spores)Angular unconformity on Cheverie Formation, Devonian granitoids and Meguma Groupundivided, 700-1500 mmudstone, sandstone, minor gypsum and shallow marine limestone, 300-800 m (Visean (Holkerian-Asbian), C-E subzones fauna and spores)bhalite, anhydrite, gypsum and mudstone, 300-500 m (Visean (Holkerian), B subzone fauna and spores)}anhydrite, salt, marine dolostone and limestone (Visean (Arundian), A subzone fauna and spores)Disconformable on Horton Group)see individual listings for ECWm and ECWlmudstone, sandstone, minor conglomerate, gypsum and shallow marine limestone, 100-700 m (Visean (Holkerian-Asbian), C-E subzones fauna and spores) Conformable-disconformable on Middle Windsor Grouphalite, anhydrite, gypsum, mudstone, siltstone, sandstone, conglomerate, 300 m (Visean (Holkerian), B subzone fauna and spores) Conformable-disconformable on Lower Windsor Groupvanhydrite, salt, gypsum, shale, marine dolostone and limestone, >150 m (Visean (Arundian), A subzone fauna and spores)fsee individual listings for ECWm and ECWl Disconformable-unconformable on Horton Group and older rocksundivided, 0-1650 mfluvial conglomerate, sandstone and minor shale, 0->100 m (Tournaisian (Courceyan) (Tn3-?V1/2) spores and fauna) Unconformable on Meguma Groupfluvial arkose, sandstone, siltstone and conglomerate, >250 m (Tournaisian (Courceyan) (Tn3) spores and fauna) Unconformable on Horton Bluff Formationfluvial-lacustrine, shale, siltstone, sandstone, conglomerate, breccia, minor dolostone and limestone, 900-1400 m (Famennian-Tournaisian (Strunian-Courceyan) (Tn1b-Tn3) spores and fauna) Unconformable on Devonian granitoids and Meguma Groupjfluvial sandstone, siltstone, conglomerate, shale, limestone, >206 m (Courceyan-Chadian (Tn3-V1/2) spores)/alluvial conglomerate, wacke, siltstone, 1600 malluvial wacke, siltstone, conglomerate, fluvial argillite, rare lacustrine limestone and felsic volcanic rocks, 1200 m (Tournaisian spores)Halluvial conglomerate, wacke, sandstone, fluvial siltstone and argillitevfluvial-lacustrine sandstone, siltstone, shale, oolitic-stromatolitic limestone, 100-1000 m (Courceyan-Chadian spores)>fluvial sandstone, minor shale, 100-500 m (Tournaisian spores)0fluvial-alluvial sandstone, conglomerate, 1500 m#alluvial conglomerate and sandstoneAbasalt, wacke, siltstone, rhyolite (Famennian-Tournaisian spores)qfelsic volcanic rocks, minor siltstone, wacke (Rb-Sr whole rock isochron ages of 387+/-2 and 341+/-4 Ma(11, 45) )4siltstone, sandstone, wacke, conglomerate, dolostone conglomerateNbasalt, andesite, rhyolite, tuff (U-Pb concordant zircon age of 389+/-2 Ma(7)),conglomerate, mudstone, siltstone, sandstone,basalt, rhyolite, tuff, sandstone, siltstonealluvial conglomerate, arkose, shale, tholeiitic basalt (Middle-Late Devonian spores) Unconformable on Knoydart and Stonehouse Formationszsiltstone, shale, conglomerate, wacke (late Emsian-early Eifelian plants) Unconformable on Silurian Wilson Brook Formationtholeiitic-alkalic basalt, rhyolite, fluvial-alluvial sandstone, conglomerate, 400-800 m (Late Devonian spores; Rb-Sr whole rock isochron age of 376+/-12 Ma(12, 37); U-Pb concordant zircon age of 373+/-4 Ma(3))OParagneiss: sillimanite-garnet+cordierite quartzo-feldspathic gneiss and schistOrthogneiss: garnet-hornblende gneiss, quartzo-feldspathic augen gneiss (40Ar/39Ar total-gas ages < on hornblende and mica of 377-371 Ma(38); Complex intruded Meguma Group)nalluvial-fluvial conglomerate, arkose, shale, felsic tuff (late Early Devonian - early Middle Devonian spores)siltstone and wackeshallow marine-subaerial silty mudstone, mudstone, shale, siltstone, sandstone, iron formation, and minor silty limestone, >1300 m (Early Lochkovian-Pragian and possibly Emsian shelly fauna of Rhenish-Bohemian affinity; late Emsian - early Eifelian plantNshallow marine-nonmarine mudstone and siltstone, >500 m (Early Devonian fauna)subaerial-shallow marine siltstone, mudstone, shale, minor limestone, arkose and rhyolite, 930 m (early Llandovery-early Gedinnian fauna)subaerial sandstone, arkose, conglomerate, siltstone, tholeiitic basalt, rhyolite, tuff, 200->400 m (Rb-Sr whole rock isochron age of 425+/-37 Ma(42)) Unconformable on Cambro-Ordovician and Neoproterozoic rocksmetamorphosed felsic and mafic volcanic and volcaniclastic rocks, slate, phyllite, psammite (Rb-Sr whole rock isochron age of 412+/-15 Ma(35); cut by Cameron Brook Pluton with U-Pb concordant zircon age of 402+/-3 Ma(19))Wshallow marine siltstone, shale, wacke, felsic volcanic rocks (Llandovery-Ludlow fauna)9shallow marine siltstone and wacke (Wenlock-Ludlow fauna)wacke, siltstone, shale, tuffpshallow marine breccia, siltstone, slate, limestone, bimodal volcanic rocks, >300 m (Late Silurian shelly fauna)[shallow marine slate, silty slate, siltstone and limestone, 0-650 m (Ludlovian graptolites)nparalic-nearshore marine quartzite, conglomerate, siltstone, slate with rhyolite and basalt at base, 30-1000 mbimodal tholeiitic-alkalic lavas and volcaniclastic rocks, 4500(?) m, at Yarmouth and Cape St. Mary Conformable-disconformable on Halifax Formationfelsic-intermediate flows and pyroclastic rocks, minor slate, conglomerate (U-Pb concordant zircon age from rhyolite of 433+7/-4 Ma(19))Rundivided (U-Pb concordant zircon age from feeder dyke(?) in 3g of 439+/-7 Ma(14))Dmetamorphosed siltstone, wacke, conglomerate, arkose, minor rhyoliteQmetamorphosed basalt, lapilli tuff, chlorite schist, pelitic and psammitic schistmetavolcanic rocks: amphibolite, hornblende-biotite schist, metarhyolite (U-Pb concordant zircon age from rhyolite of 428+/-4 Ma(30))]metasedimentary rocks: semipelitic schist, pelitic schist, calcsilicate rocks and rare marbleorthogneiss, minor semipelitic paragneiss and biotite schist (U-Pb concordant zircon age from orthogneiss of 396+/-2 Ma(19)) Unconformable on McMillan Flowage Formation8psammitic-pelitic gneiss and schist, marble, amphibolite>psammitic, semipelitic and pelitic gneiss, marble, amphiboliteJsemipelitic, pelitic and calcsilicate gneiss, minor marble and amphibolite3amphibolitic metavolcanic and metasedimentary rocksTmarine shale, >400 m (Tremadocian-Arenigian graptolites, trilobites and brachiopods)slope-outer shelf slate, siltstone, minor sandstone and Fe-Mn nodules (in places metamorphosed to schist), 500->4400 m (Tremadocian graptolites and acritarchs)]sandstone turbidites and slate, 0-870 m (Middle Cambrian trilobites of Acado-Baltic affinity)sandstone turbidites and slate: continental rise prism (in places metamorphosed to schist and gneiss), >5600 m (U-Pb concordant zircon and detrital titanite ages near base and top of unit of 566+/-8 and 552+/-5 Ma(39) respectively)alluvial-fluvial conglomerate, sandstone and shale, shallow marine limestone, shale, ironstone, quartzite and tuff, >800 m (Early Cambrian (Tommotian-Botomian) - Early Ordovician trilobites and other fauna)tholeiitic basalt, rhyolite, tuff, siltstone, shale, 200-700 m (early Middle Cambrian fauna) (U-Pb concordant zircon age of 505+/-3 Ma(47)) Unconformable on George River Metamorphic Suitemarine shale and limestone, >100-300 m (Late Cambrian trilobites and brachiopods)Disconformable on MacMullin and MacLean Brook FormationsMshallow marine siltstone and shale, >300 m (early Middle Cambrian trilobites)\shallow marine siltstone and shale, >300 m (late Middle Cambrian brachiopods and trilobites)Fmarine shale, 170 m (early Middle Cambrian trilobites and brachiopods)alluvial-fluvial conglomerate, sandstone and shale, shallow marine alkalic basalt, rhyolite, tuff, shale and limestone, >1200 m (pebbles of Early Cambrian (Tommotian-Botomian) trilobites and other fauna in upper member of Arbuckle Brook Formation) Unconfshallow marine siltstone, shale, mudstone, >500 m (= Bonavista Group and Brigus Formation, Newfoundland) (Early Cambrian (Tommotian-Botomian) trilobites and brachiopods)prodeltaic-macrotidal conglomerate, sandstone and siltstone, shallow marine quartzite, >300 m (= Chapel Island and Random Formations of Manykaian age in Newfoundland)|subaerial-tidal arkose, conglomerate and siltstone, >500 m (= Rencontre Formation of latest Proterozoic age in Newfoundland)felsic-intermediate tuff, tholeiitic volcanic arc basalt, conglomerate, arkose, sandstone, siltstone (U-Pb discordant zircon age of 600 m (cut by Debert River granite with a U-Pb concordant zircon age of 609+/-4 Ma(16)) Unconformable on deformed Gamble Brook FormationCranberry Lake Formation: metamorphosed, deep marine, arkosic turbidites, >200 m; Humming Brook Formation: metamorphosed argillite, rare sandstone and siltstone, >100 m; Gilbert Hills Formation: metamorphosed tholeiitic and calcalkaline, felsic-intermediCmetamorphosed felsic-mafic lavas and pyroclastics, turbiditic wackegmetamorphosed tholeiitic and calcalkaline, mafic-felsic lavas and tuffs, turbiditic wacke and argillite3deep water laminated mudstone and siltstone, >200 m9tholeiitic ocean island basalt, wacke and mudstone, 400 mLdeep water, turbiditic conglomerate, wacke, mudstone and minor basalt, 600 m3deep water mudstone, siltstone and turbiditic wacketholeiitic and calcalkaline, mafic-intermediate-felsic flows and tuffs, siltstone, slate, wacke, >2200 m (U-Pb concordant zircon and monazite age of 618+/-2 Ma(41))odeep water turbiditic conglomerate, mudstone, 700(?) m (U-Pb age of youngest detrital zircon of 613+/-5 Ma(36))deep water mudstone, minor wacke, chert, limestone, 700(?) m (cut by Greendale Pluton with a U-Pb concordant zircon age of 607+/-2 Ma(41))Mtholeiitic and calcalkaline mafic flows and tuffs, marble, mudstone, 600(?) m-felsic, intermediate and mafic tuffs or flowsfelsic, intermediate and mafic tuff, calcalkaline volcanic arc basalt, andesite, rhyolite, conglomerate, sandstone, siltstone (U-Pb concordant zircon ages of 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@@@>08888888888888888888888888888>@A @;;;7 Oh+'0HPdx  Greg Kehm  Greg Kehm Microsoft Excel@{rN@*oN@DN՜.+,0 PXx  The Nature Conservancys: READMESheet1  Worksheets  !"#$%&'()*+,-./0123456789:;<=>?@ABCDEFGHIJKLMNOPQRSTUVWXZ[\]^_`bcdefghRoot Entry FWorkbookYSummaryInformation(YDocumentSummaryInformation8a