Lontova Formation | Stratigraphy

Stratigraphy

Lontova Formation

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Number	Name	Locality	Depth (m)		Stratigraphy	Image
Number	Name	Locality	From	To	Stratigraphy	Image
GIT 293-206-2		Mudamõisa F-234 borehole	129.60		Lontova Stage
GIT 293-17-2	Sabellidites cambriensis	Aseri 249 borehole	85.10		Lontova Stage
GIT 293-17-1	Sabellidites cambriensis	Aseri 249 borehole	85.10		Lontova Stage
GIT 293-15-5	Sabellidites cambriensis	Kunda 62 borehole	53.50		Lontova Stage
GIT 293-15-4	Sabellidites cambriensis	Kunda 62 borehole	53.50		Lontova Stage
GIT 293-15-3	Sabellidites cambriensis	Kunda 62 borehole	53.50		Lontova Stage
GIT 293-15-2	Sabellidites cambriensis	Kunda 62 borehole	53.50		Lontova Stage
GIT 293-26-1	Sabellidites cambriensis	Korõtno 2 borehole	406.00		Lontova Stage	+1
GIT 293-55-2	Hyolithellus	Kunda quarry			Lontova Stage
GIT 293-83-6	Conotubus	Kunda quarry			Lontova Stage
GIT 293-190-3	Conotubus hemiannulatus	Imastu F-140 borehole	188.00		Lontova Stage
GIT 293-190-2	Platysolenites antiquissimus	Imastu F-140 borehole	188.00		Lontova Stage
GIT 293-66-2	Bioturbation trace fossils	Imastu F-140 borehole	188.00	188.90	Lontova Stage
GIT 293-194-3	Hyolitha	Vanamõisa F-149 borehole, Lääne-Virumaa	99.60		Lontova Stage
GIT 293-194-2	Hyolitha	Vanamõisa F-149 borehole, Lääne-Virumaa	99.60		Lontova Stage
GIT 293-201-3	Planolites	Elva 555 borehole	470.00		Lontova Stage
GIT 293-201-2	Protohertzina	Elva 555 borehole	470.00		Lontova Stage
GIT 293-197-2	Planolites	Vanamõisa F-149 borehole, Lääne-Virumaa	150.60		Lontova Stage
GIT 293-309-1	Sabellidites	Haapsalu 203 borehole	218.00
GIT 293-294-2	Incertae sedis (fossils)	Uhtna 320 borehole	185.00		Baltic Lower Cambrian
GIT 293-48-2	Platysolenites spiralis	Tammneeme outcrop			Lontova Stage
GIT 293-44-3	Platysolenites antiquissimus	Tammneeme outcrop			Lontova Stage
GIT 293-44-2	Platysolenites antiquissimus	Tammneeme outcrop			Lontova Stage
GIT 293-39-2	Platysolenites antiquissimus	Laitse 6 borehole	134.00	134.40	Lontova Stage
GIT 293-37-3	Hyolitha	Metsiku F-135 borehole	-53.50		Lontova Stage

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