arkL edit interval

arkL

select id,columnx from arkL_columns where dataset_id like 80

View/Edit arkL Database interval - Xinyuan Fm. (Guandao)

Navigation

The age-window currently being used to search for terms for autocompletion is 191.46 -> 296.59 Ma.

	interval above:	Guanling Fm. (Guanling)
parent-intervals:Guandao region, Guizhou (South margin of Yangtze platform);	this interval:	Xinyuan Fm. (Guandao)	sub-intervals:
	interval below:	Green Bean Rock

Mode selector

Interval data

intervalx:	Xinyuan Fm. (Guandao)has added abv?id: 7323 sort:200
alternative_term:	block label:
formal term:
interval_type:
parent_interval:
dataset:	strat - Yangtse Platform (China, Tr) (dataset id = 80)
alt dataset:	(dataset id = 0)
TSC Column:	id:169
stage:
colour:
interval_notes:	Schematically, the thickest carbonate debris flow at Guandao is shown here -- for graphic purposes, it is shown as spanning 0.5 myr (0.25 on either side of the MT4r/MT4n polarity boundary; although it would be an instantaneous event.
compilation_notes:
refs to add:
linked refs:
preset_duration:
preset_duration_notes:
tracecode	; Q2top from event age; Q1base from event age; Q3a duration from base & top

	age2020	age		event	event_id	pup	in interval	age	age2020
Top:		241.4600	<---	base Guanling Fm. (Guanling)	9413	0.0000	Ladinian	241.46	00241.4600
Base:		246.5900	<---	base Xinyuan Fm. (Guandao)	9423	0.0000	MT3n	246.59	00246.5500
base notes	In the Anisian, the Guandao succession has facies of "deep-marine slope sedimentation consisting of pelagic lime-mudstone punctuated by carbonate packstone–grainstone turbidite and debris flow breccia beds." (Lehrmann et al., 2015). Change in facies at Wantao is essentially base of the MT3n polarity zone (used here).				comp notes

if you were a logged in editor there would be an input button here

Interval References

Dataset References