/* DATA DESCRIPTION:
Citation:	Vetó, István; Hetényi, Magdolna; Demény, Attila; Hertelendi, Ede (1994): Geochemistry and degree of organic carbon preservation in non-bioturbated, shaly sediments [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.763277, 
	Supplement to: Vetó, I et al. (1994): Hydrogen index as reflecting intensity of suiphidic diagenesis in non-bioturbated, shaly sediments. Organic Geochemistry, 22(2), 299-310, https://doi.org/10.1016/0146-6380(94)90176-7
Abstract:	Based on 13 published porewater H2S and sulphate profiles the amount of H2S escaping from non-bioturbated shales varies between some few % to 45% of the amount of bacterially generated H2S. This finding permits calculation of the original organic carbon (TOCor) content of immature nonbioturbated shales using TOC and sulphur content data. In two immature non-bioturbated sequences from Hungary (Toarcian and Oligocene) the first-order correlation between HI and TOC/TOCor was found to be stronger than that between HI and TOC, indicating that sulphate reduction was the leading process both in decrease in TOC content and degradation of kerogen source potential.
Project(s):	Ocean Drilling Program (ODP) (URI: https://www-odp.tamu.edu:443/)
Coverage:	MEDIAN LATITUDE: 27.611167 * MEDIAN LONGITUDE: -14.154057 * SOUTH-BOUND LATITUDE: -11.266500 * WEST-BOUND LONGITUDE: -79.062170 * NORTH-BOUND LATITUDE: 47.100000 * EAST-BOUND LONGITUDE: 19.000000
	DATE/TIME START: 1986-11-09T01:15:00 * DATE/TIME END: 1986-11-14T13:30:00
Event(s):	112-682A * LATITUDE: -11.266500 * LONGITUDE: -79.062170 * DATE/TIME START: 1986-11-09T01:15:00 * DATE/TIME END: 1986-11-14T13:30:00 * ELEVATION: -3801.0 m * Penetration: 436.7 m * Recovery: 127.04 m * LOCATION: South Pacific Ocean * CAMPAIGN: Leg112 (URI: https://doi.org/10.2973/odp.proc.ir.112.1988) * BASIS: Joides Resolution (URI: https://www-odp.tamu.edu:443/resolutn.html) * METHOD/DEVICE: Drilling/drill rig (DRILL) * COMMENT: 48 cores; 436.7 m cored; 0 m drilled; 29.1 % recovery
	Urkut_ore_mine * LATITUDE: 47.100000 * LONGITUDE: 17.600000 * METHOD/DEVICE: Sampling by hand (HAND) * COMMENT: Position estimated
	Wall_Ad3 * LATITUDE: 47.000000 * LONGITUDE: 19.000000 * METHOD/DEVICE: Drilling/drill rig (DRILL) * COMMENT: Position estimated, well near Budapest
License:	Creative Commons Attribution 3.0 Unported (CC-BY-3.0) (URI: https://creativecommons.org/licenses/by/3.0/)
Size:	3 datasets
*/
/* TABULAR SUMMARY OF DATASETS LISTED IN THIS COLLECTION: */
Filename	Citation of child dataset
112-682A_carbon_chem.tab	Vetó, István; Hetényi, Magdolna; Demény, Attila; Hertelendi, Ede (1994): (Table 7) Geochemistry and degree of organic carbon preservation in the Oligocene-lower Miocene sequence of ODP Hole 112-682A. https://doi.org/10.1594/PANGAEA.763276
Urkut_ore_mine_carbon_chem.tab	Vetó, István; Hetényi, Magdolna; Demény, Attila; Hertelendi, Ede (1994): (Table 5) Geochemistry and degree of organic carbon preservation in the Toarcian radiolarian marl, Urkut Mn-ore mine. https://doi.org/10.1594/PANGAEA.763275
Wall_Ad3_carbon_chem.tab	Vetó, István; Hetényi, Magdolna; Demény, Attila; Hertelendi, Ede (1994): (Table 6) Geochemistry and degree of organic carbon preservation in the laminated part of the Tard Clay, well Ad 3. https://doi.org/10.1594/PANGAEA.763274
