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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| creator | 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 |
| description | 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_str_mv | 10.5281/zenodo.14179032 |
| format | Dataset |
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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.</description><subject>continent-ocean transition</subject><subject>continental breakup</subject><subject>crustal architecture</subject><subject>earth connections</subject><subject>Expedition 349</subject><subject>Expedition 367</subject><subject>Expedition 367/368</subject><subject>Expedition 368</subject><subject>Expedition 368X</subject><subject>hyperextension</subject><subject>International Ocean Discovery Program</subject><subject>IODP</subject><subject>JOIDES Resolution</subject><subject>Leg 184</subject><subject>lithosphere thinning</subject><subject>northern South China Sea</subject><subject>outer margin high</subject><subject>paleo-ice sheet</subject><subject>paleoclimate</subject><subject>rifted margin</subject><subject>Site U1499</subject><subject>Site U1500</subject><subject>Site U1501</subject><subject>Site U1502</subject><subject>Site U1503</subject><subject>Site U1504</subject><subject>Site 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Expedition 367 Elemental analysis (CHNS)</title><author>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, 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C.</creatorcontrib><creatorcontrib>Skinner, Steven M.</creatorcontrib><creatorcontrib>Straub, Susanne M.</creatorcontrib><creatorcontrib>Su, Chih C.</creatorcontrib><creatorcontrib>Su, Xiang</creatorcontrib><creatorcontrib>Tian, Liyan</creatorcontrib><creatorcontrib>van der Zwan, Froukie M.</creatorcontrib><creatorcontrib>Wan, Shiming</creatorcontrib><creatorcontrib>Wu, Huaichun</creatorcontrib><creatorcontrib>Xiang, Rong</creatorcontrib><creatorcontrib>Yadav, Rajeev</creatorcontrib><creatorcontrib>Yi, Liang</creatorcontrib><creatorcontrib>Zhang, Cuimei</creatorcontrib><creatorcontrib>Zhang, Jinchang</creatorcontrib><creatorcontrib>Zhang, Yang</creatorcontrib><creatorcontrib>Zhao, Ning</creatorcontrib><creatorcontrib>Zhong, Guangfa</creatorcontrib><creatorcontrib>Zhong, Lifeng</creatorcontrib><collection>DataCite (Open Access)</collection><collection>DataCite</collection></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext_linktorsrc</fulltext></delivery><addata><au>Larsen, Hans Christian</au><au>Sun, Zhen</au><au>Stock, Joann M.</au><au>Jian, Zhimin</au><au>Alvarez Zarikian, Carlos A.</au><au>Klaus, Adam</au><au>Boaga, Jacopo</au><au>Bowden, Stephen A.</au><au>Briais, Anne</au><au>Chen, Yifeng</au><au>Childress, Laurel B.</au><au>Cukur, Deniz</au><au>Dadd, Kelsie A.</au><au>Deng, Jia-Ming</au><au>Ding, Weiwei</au><au>Dorais, Michael J.</au><au>Ferre, Eric C.</au><au>Ferreira, Fabricio</au><au>Furusawa, Akira</au><au>Gewecke, Aaron J.</au><au>Hinojosa, Jessica L.</au><au>Hofig, Tobias W.</au><au>Hsiung, Kan His</au><au>Huang, Baoqi</au><au>Huang, Enqing</au><au>Huang, Xiao Long</au><au>Jiang, Shijun</au><au>Jin, Haiyan</au><au>Johnson, Benjamin G.</au><au>Kurzawski, Robert M.</au><au>Lei, Chao</au><au>Li, Baohua</au><au>Li, Li</au><au>Li, Yanping</au><au>Lin, Jian</au><au>Liu, Chang</au><au>Liu, Chuanlian</au><au>Liu, Zhifei</au><au>Luna, Antonio</au><au>Lupi, Claudia</au><au>McCarthy, Anders J.</au><au>McIntosh, Kirk</au><au>Mohn, Geoffroy</au><au>Ningthoujam, Lachit Singh</au><au>Nirrengarten, Michael F.R.</au><au>Osono, Nobuaki</au><au>Peate, David W.</au><au>Persaud, Patricia</au><au>Qiu, Ning</au><au>Robinson, Caroline M.</au><au>Satolli, Sara</au><au>Sauermilch, Isabel</au><au>Schindlbeck, Julie C.</au><au>Skinner, Steven M.</au><au>Straub, Susanne M.</au><au>Su, Chih C.</au><au>Su, Xiang</au><au>Tian, Liyan</au><au>van der Zwan, Froukie M.</au><au>Wan, Shiming</au><au>Wu, Huaichun</au><au>Xiang, Rong</au><au>Yadav, Rajeev</au><au>Yi, Liang</au><au>Zhang, Cuimei</au><au>Zhang, Jinchang</au><au>Zhang, Yang</au><au>Zhao, Ning</au><au>Zhong, Guangfa</au><au>Zhong, Lifeng</au><format>book</format><genre>unknown</genre><ristype>DATA</ristype><title>IODP Expedition 367 Elemental analysis (CHNS)</title><date>2018-09-28</date><risdate>2018</risdate><abstract>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.</abstract><pub>International Ocean Discovery Program</pub><doi>10.5281/zenodo.14179032</doi><orcidid>https://orcid.org/0000-0002-9691-3570</orcidid><orcidid>https://orcid.org/0000-0003-2377-2866</orcidid><orcidid>https://orcid.org/0000-0003-1570-760X</orcidid><orcidid>https://orcid.org/0000-0003-2131-9072</orcidid><orcidid>https://orcid.org/0000-0002-0040-6348</orcidid><orcidid>https://orcid.org/0000-0002-1936-8978</orcidid><orcidid>https://orcid.org/0000-0003-4983-050X</orcidid><orcidid>https://orcid.org/0000-0001-8588-3962</orcidid><orcidid>https://orcid.org/0000-0002-9462-9322</orcidid><orcidid>https://orcid.org/0000-0001-5865-3272</orcidid><orcidid>https://orcid.org/0000-0002-1381-7904</orcidid><orcidid>https://orcid.org/0000-0003-2552-0144</orcidid><orcidid>https://orcid.org/0000-0002-7813-5824</orcidid><orcidid>https://orcid.org/0000-0001-6429-9791</orcidid><orcidid>https://orcid.org/0000-0002-3785-3336</orcidid><orcidid>https://orcid.org/0000-0002-6228-506X</orcidid><orcidid>https://orcid.org/0000-0002-3741-6371</orcidid><orcidid>https://orcid.org/0000-0002-7708-0788</orcidid><orcidid>https://orcid.org/0000-0002-2991-9999</orcidid><orcidid>https://orcid.org/0000-0001-9503-7970</orcidid><orcidid>https://orcid.org/0000-0001-9335-2248</orcidid><orcidid>https://orcid.org/0000-0002-6625-0913</orcidid><orcidid>https://orcid.org/0000-0001-6259-7912</orcidid><orcidid>https://orcid.org/0000-0002-3637-8609</orcidid><orcidid>https://orcid.org/0000-0003-3462-7023</orcidid><orcidid>https://orcid.org/0000-0001-9489-5738</orcidid><orcidid>https://orcid.org/0000-0002-7624-1607</orcidid><orcidid>https://orcid.org/0000-0001-9848-9745</orcidid><orcidid>https://orcid.org/0000-0002-6268-6592</orcidid><orcidid>https://orcid.org/0000-0003-2826-1897</orcidid><orcidid>https://orcid.org/0000-0002-9795-9239</orcidid><orcidid>https://orcid.org/0000-0002-8589-102X</orcidid><orcidid>https://orcid.org/0000-0002-9254-4528</orcidid><orcidid>https://orcid.org/0000-0002-9944-2356</orcidid><orcidid>https://orcid.org/0000-0003-4816-7865</orcidid><orcidid>https://orcid.org/0000-0001-9811-4409</orcidid><orcidid>https://orcid.org/0000-0002-2177-2742</orcidid><orcidid>https://orcid.org/0000-0002-8729-2960</orcidid><orcidid>https://orcid.org/0000-0003-0437-3456</orcidid><oa>free_for_read</oa></addata></record> |
| fulltext | fulltext_linktorsrc |
| identifier | DOI: 10.5281/zenodo.14179032 |
| ispartof | |
| issn | |
| language | eng |
| recordid | cdi_datacite_primary_10_5281_zenodo_14179032 |
| source | DataCite |
| subjects | 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 |
| title | IODP Expedition 367 Elemental analysis (CHNS) |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-16T00%3A40%3A00IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-datacite_PQ8&rft_val_fmt=info:ofi/fmt:kev:mtx:book&rft.genre=unknown&rft.au=Larsen,%20Hans%20Christian&rft.date=2018-09-28&rft_id=info:doi/10.5281/zenodo.14179032&rft_dat=%3Cdatacite_PQ8%3E10_5281_zenodo_14179032%3C/datacite_PQ8%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_id=info:pmid/&rfr_iscdi=true |