{"corpus_id":188828751,"paper_sha":"e5a8d58b5fea5d7fb57fbf103c75b0cc661c91f8","doi":"10.3285/EG.27.1.09","arxiv_id":null,"pmid":null,"pmcid":null,"mag_id":2790530877,"dblp_id":null,"acl_id":null,"title":"Quartärgliederung und Aufbau von Warmzeit-Kaltzeit-Zyklen in Bereichen mit Dominanz periglazialer Hangsedimente, dargestellt am Quartärprofil Dreihausen/Hessen","year":1976,"publication_date":null,"venue":"","journal":{"name":"EG Quaternary Science Journal","pages":"93-120","volume":"27"},"journal_issn":null,"journal_title":null,"publication_types":[],"pubmed_pub_types":null,"s2_fields_of_study":[],"reference_count":4,"citation_count":10,"influential_citation_count":0,"is_open_access":true,"arxiv_categories":null,"arxiv_license":null,"arxiv_journal_ref":null,"mesh_headings":null,"chemicals":null,"comments_corrections":null,"source_flags":1,"s2_open_access_pdf_url":"https://www.eg-quaternary-sci-j.net/27/93/1976/egqsj-27-93-1976.pdf","s2_open_access_landing_url":"https://www.semanticscholar.org/paper/e5a8d58b5fea5d7fb57fbf103c75b0cc661c91f8","s2_open_access_license":"CCBY","s2_open_access_status":"HYBRID","pmc_open_access_pdf_url":null,"pmc_open_access_landing_url":null,"pmc_open_access_license":null,"pmc_open_access_status":null,"unpaywall_open_access_pdf_url":null,"unpaywall_open_access_landing_url":null,"unpaywall_open_access_license":null,"unpaywall_open_access_status":null,"abstract":"Das Quartarprofil Dreihausen/Hessen ist durch Verzahnung von Los bzw. Loslehm und periglazialen Hangsedimenten gekennzeichnet. Der uber 12 m hohe Aufschlus wurde geomorphologisch, stratigraphisch und mikromorphologisch untersucht. Es konnen 13 Bodenbildungs-Sedimentations-Zyklen unterschieden werden. Aufgrund der erzielten Ergebnisse wird das Idealbild eines quartaren Warmzeit-Kaltzeit-Zyklus entworfen.","claims":[{"public_id":"cl_3a0323f74ae08f379168fb20f53d120e","status":"active","text":"Based on the results, an ideal model of a Quaternary warm-cold cycle is designed.","confidence":0.9,"contributors":[{"id":32,"public_id":"7c402c1b98","public_label":"뀨 (7c402c1b98)","roles":["extraction"],"url":"https://sah.borca.ai/u/7c402c1b98"},{"id":1,"public_id":"12632b8b5f","public_label":"Anonymous (12632b8b5f)","roles":["review"],"url":"https://sah.borca.ai/u/12632b8b5f"}],"url":"https://sah.borca.ai/claims/cl_3a0323f74ae08f379168fb20f53d120e"},{"public_id":"cl_dd46860ad539a466cd197f798593f007","status":"active","text":"The Dreihausen/Hessen Quaternary profile is characterized by interlocking of loess/loess loam and periglacial slope sediments, and 13 pedogenesis-sedimentation cycles can be 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