MOLAR-TOOTH STRUCTURE IN PROTEROZOIC CARBONATE ROCKS - ORIGIN FROM SYNSEDIMENTARY EARTHQUAKES, AND IMPLICATIONS FOR THE NATURE AND EVOLUTION OF BASINS AND MARINE SEDIMENT
Br. Pratt, MOLAR-TOOTH STRUCTURE IN PROTEROZOIC CARBONATE ROCKS - ORIGIN FROM SYNSEDIMENTARY EARTHQUAKES, AND IMPLICATIONS FOR THE NATURE AND EVOLUTION OF BASINS AND MARINE SEDIMENT, Geological Society of America bulletin, 110(8), 1998, pp. 1028-1045
Proterozoic argillaceous lime mudstones commonly contain molar-tooth s
tructure, a curious synsedimentary feature consisting of crumpled, gen
erally vertically oriented veins filled with calcite microspar. Long e
nigmatic, these veins are interpreted here as earthquake-induced defor
mation structures. A model is proposed whereby violent ground motion c
aused shrinkage, dewatering, and fissuring of the colloidal sea-floor
sediment of clay and lime mud, A slurry of equant particles of lime mu
d, segregated from the clay platelets trapped in the matrix, was expel
led into these voids. The host bed underwent as much as 80% compaction
as well as shear, causing the lime mud-filled fissures to be ptygmati
cally folded and shingled both vertically and horizontally, and in pla
ces pulled apart. This lime mud lithified rapidly by high-Mg calcite g
rain growth, such that subsequent earthquakes shattered the folded vei
ns. In the Belt basin of western North America, tsunamis from differen
t events created currents that transported ooids and coarse sand from
shoals into deeper water, and scoured deeply into the now-consolidated
sediment, leaving behind a lag of vein fragments,Molar-tooth structur
e is a signature of basin tectonism recorded specifically in argillace
ous Lime mudstones deposited in low-energy settings above the thermocl
ine in supersaturated marine water. Syneresis cracks are the counterpa
rt in terrigenous facies, in that silt and sand were injected into the
shrinkage fissures. This process points to the importance of seismica
lly induced compaction under negligible burial. Smectite might have ma
de up a significant proportion of the sediment making it more conduciv
e to shrinkage. The absence of molar-tooth structure in Phanerozoic st
rata is ascribed mainly to changes in sediment rheology brought about
by increased organic binding due to diversification of the microbiota.