lesson 12: sedimentary iron deposits Flashcards
at least how many percent of iron are SIDs?
> 15%
range of iron for SIDs during the mostly distribution periods?
24-40%
explain the obvious distinction between iron rocks and iron stones
iron stones are the more modern occurrences that are nodular in texture, iron stones are the ones formed during the precambrian that are laminated or banded
describe iron rocks
—precambrian
— >15% iron
—laminated
—thin bedded
—commonly cherty (not necessarily tho)
periods of distribution for SIDs
—precambrian
—phanerozoic
—paleozoic
—jurassic
—cretaceous
describe iron stones
— >15% Fe
—non laminated
—non cherty
—lower silica
—typically oolitic
peak distribution of iron rocks
precambrian to devonian
—mid archean
—early proterozoic
—late proterozoic
describe the spatial distribution or iron rocks
—mostly continental (old rocks)
—cratons formerly covered by the sea (cherty and sed) but then got uplifted after some time
describe the mineralogy of SIDs
the rocks are commonly grouped based on their mineralogy
—oxides (hematitic, magnetitic)
—silicates (minnesotaite)
—carbonates (siderite)
—sulfates (pyrite)
describe the structures of SIDs
—microbands (mm)
—mesobands (cm)
—chert matrix
—granule iron formation
separation of iron bands by cherty material (sandwiched between them)
chert matrix
non banded iron formation structures
granule iron formation
structures that only apply to iron rocks
—microbands
—mesobands
—chert matrix
what are the three associated facies for iron rocks
—Algoma type
—Superior type
—Raritan type
facies that are thinly bedded, near volcanoes, volcanic related (pyroclastics), near MORs, explosive occurrences, lack oolitic, granular
Algoma type
facies with no volcanic associations
Superior type
superior type facies occur with?
quartzite, black carbonaceous shales, conglomerate, dolomite, cherts, breccia, argillites
facies related to glacial deposits
raritan type
iron stone facies
—sandy and shelly
—ferric oxide
facies that are shallow marine sediments with abundant pellets of glauconite (green if not oxidized)
sandy and shelly iron stone facie
facie that include chamosite (iron chlorite), oolite, and can include hematite and geothite
ferric oxide
minerals that are associated with something being weathered
ferric oxides (esp geothite)
usually if fresh thered be magnetite, biotite, pyrite. but then if weathered, magnetite and biotite actually turns into geothite
structures commonly found in iron stones (8)
—commonly interbedded with carbonates
—cross beds
—scour and fill
—rip-up clasts
—burrows
—shallow marine
—deltaic
—pelagic sediments
nonferrous associations of iron stones
detrital quartz, calcite, dolomite, authigenic phospherite, authigenic chert