IODP Expedition 367 Elemental analysis (CHNS)

Fundamental elemental component (total carbon, hydrogen, nitrogen, and sulfur) fluctuations help define the origin, depositional environment, and diagenetic alteration of source materials. To determine C, H, N, and S, solid samples are reacted with a catalyst, separated by chromatography, and detect...

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Hauptverfasser:	Larsen, Hans Christian, Sun, Zhen, Stock, Joann M., Jian, Zhimin, Alvarez Zarikian, Carlos A., Klaus, Adam, Boaga, Jacopo, Bowden, Stephen A., Briais, Anne, Chen, Yifeng, Childress, Laurel B., Cukur, Deniz, Dadd, Kelsie A., Deng, Jia-Ming, Ding, Weiwei, Dorais, Michael J., Ferre, Eric C., Ferreira, Fabricio, Furusawa, Akira, Gewecke, Aaron J., Hinojosa, Jessica L., Hofig, Tobias W., Hsiung, Kan His, Huang, Baoqi, Huang, Enqing, Huang, Xiao Long, Jiang, Shijun, Jin, Haiyan, Johnson, Benjamin G., Kurzawski, Robert M., Lei, Chao, Li, Baohua, Li, Li, Li, Yanping, Lin, Jian, Liu, Chang, Liu, Chuanlian, Liu, Zhifei, Luna, Antonio, Lupi, Claudia, McCarthy, Anders J., McIntosh, Kirk, Mohn, Geoffroy, Ningthoujam, Lachit Singh, Nirrengarten, Michael F.R., Osono, Nobuaki, Peate, David W., Persaud, Patricia, Qiu, Ning, Robinson, Caroline M., Satolli, Sara, Sauermilch, Isabel, Schindlbeck, Julie C., Skinner, Steven M., Straub, Susanne M., Su, Chih C., Su, Xiang, Tian, Liyan, van der Zwan, Froukie M., Wan, Shiming, Wu, Huaichun, Xiang, Rong, Yadav, Rajeev, Yi, Liang, Zhang, Cuimei, Zhang, Jinchang, Zhang, Yang, Zhao, Ning, Zhong, Guangfa, Zhong, Lifeng
Format:	Dataset
Sprache:	eng
Schlagworte:	continent-ocean transition continental breakup crustal architecture earth connections Expedition 349 Expedition 367 Expedition 367/368 Expedition 368 Expedition 368X hyperextension International Ocean Discovery Program IODP JOIDES Resolution Leg 184 lithosphere thinning northern South China Sea outer margin high paleo-ice sheet paleoclimate rifted margin Site U1499 Site U1500 Site U1501 Site U1502 Site U1503 Site U1504 Site U1505 subsidence
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Beschreibung
Zusammenfassung:	Fundamental elemental component (total carbon, hydrogen, nitrogen, and sulfur) fluctuations help define the origin, depositional environment, and diagenetic alteration of source materials. To determine C, H, N, and S, solid samples are reacted with a catalyst, separated by chromatography, and detected by thermal conductivity on a FlashEA 1112 CHNS elemental analyzer. Organic carbon can be directly measured on the elemental analyzer by acidification of the sample to drive off carbonate as carbon dioxide before analyzing. Total organic carbon on this report is measured rather than calculated.
DOI:	10.5281/zenodo.14179032