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Evolution of solution dolines inferred from cosmogenic 36 Cl in calcite

2010; Geological Society of America; Volume: 38; Issue: 11 Linguagem: Inglês

10.1130/g31302.1

1943-2682

Yuki Matsushi, Tsuyoshi Hattanji, Sanae Akiyama, Kimikazu Sasa, Tsutomu Takahashi, Keisuke Sueki, Yukinori Matsukura,

Methane Hydrates and Related Phenomena

Research Article| November 01, 2010 Evolution of solution dolines inferred from cosmogenic 36Cl in calcite Yuki Matsushi; Yuki Matsushi * 1Disaster Prevention Research Institute, Kyoto University, Gokasho, Uji, Kyoto 611-0011, Japan *E-mail: matsushi.yuki.7w@kyoto-u.ac.jp. Search for other works by this author on: GSW Google Scholar Tsuyoshi Hattanji; Tsuyoshi Hattanji 2Graduate School of Life and Environmental Sciences, University of Tsukuba, 1-1-1 Tenno-dai, Tsukuba, Ibaraki 305-8572, Japan Search for other works by this author on: GSW Google Scholar Sanae Akiyama; Sanae Akiyama 2Graduate School of Life and Environmental Sciences, University of Tsukuba, 1-1-1 Tenno-dai, Tsukuba, Ibaraki 305-8572, Japan Search for other works by this author on: GSW Google Scholar Kimikazu Sasa; Kimikazu Sasa 3Accelerator Mass Spectrometry Group, Tandem Accelerator Complex, University of Tsukuba, 1-1-1 Tenno-dai, Tsukuba, Ibaraki 305-8577, Japan Search for other works by this author on: GSW Google Scholar Tsutomu Takahashi; Tsutomu Takahashi 3Accelerator Mass Spectrometry Group, Tandem Accelerator Complex, University of Tsukuba, 1-1-1 Tenno-dai, Tsukuba, Ibaraki 305-8577, Japan Search for other works by this author on: GSW Google Scholar Keisuke Sueki; Keisuke Sueki 3Accelerator Mass Spectrometry Group, Tandem Accelerator Complex, University of Tsukuba, 1-1-1 Tenno-dai, Tsukuba, Ibaraki 305-8577, Japan Search for other works by this author on: GSW Google Scholar Yukinori Matsukura Yukinori Matsukura 2Graduate School of Life and Environmental Sciences, University of Tsukuba, 1-1-1 Tenno-dai, Tsukuba, Ibaraki 305-8572, Japan Search for other works by this author on: GSW Google Scholar Author and Article Information Yuki Matsushi * 1Disaster Prevention Research Institute, Kyoto University, Gokasho, Uji, Kyoto 611-0011, Japan Tsuyoshi Hattanji 2Graduate School of Life and Environmental Sciences, University of Tsukuba, 1-1-1 Tenno-dai, Tsukuba, Ibaraki 305-8572, Japan Sanae Akiyama 2Graduate School of Life and Environmental Sciences, University of Tsukuba, 1-1-1 Tenno-dai, Tsukuba, Ibaraki 305-8572, Japan Kimikazu Sasa 3Accelerator Mass Spectrometry Group, Tandem Accelerator Complex, University of Tsukuba, 1-1-1 Tenno-dai, Tsukuba, Ibaraki 305-8577, Japan Tsutomu Takahashi 3Accelerator Mass Spectrometry Group, Tandem Accelerator Complex, University of Tsukuba, 1-1-1 Tenno-dai, Tsukuba, Ibaraki 305-8577, Japan Keisuke Sueki 3Accelerator Mass Spectrometry Group, Tandem Accelerator Complex, University of Tsukuba, 1-1-1 Tenno-dai, Tsukuba, Ibaraki 305-8577, Japan Yukinori Matsukura 2Graduate School of Life and Environmental Sciences, University of Tsukuba, 1-1-1 Tenno-dai, Tsukuba, Ibaraki 305-8572, Japan *E-mail: matsushi.yuki.7w@kyoto-u.ac.jp. Publisher: Geological Society of America Received: 15 Apr 2010 Revision Received: 23 Jun 2010 Accepted: 29 Jun 2010 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2010 Geological Society of America Geology (2010) 38 (11): 1039–1042. https://doi.org/10.1130/G31302.1 Article history Received: 15 Apr 2010 Revision Received: 23 Jun 2010 Accepted: 29 Jun 2010 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Yuki Matsushi, Tsuyoshi Hattanji, Sanae Akiyama, Kimikazu Sasa, Tsutomu Takahashi, Keisuke Sueki, Yukinori Matsukura; Evolution of solution dolines inferred from cosmogenic 36Cl in calcite. Geology 2010;; 38 (11): 1039–1042. doi: https://doi.org/10.1130/G31302.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Quantification of the development of solution dolines provides important information for understanding the long-term evolution of karst landscapes. This study reports the initial results of an investigation of the long-term denudation rates along the side slopes of a solution doline based on analyses of cosmogenic 36Cl in calcite. The denudation rates increase in proportion with increasing size of the topographic contributing area, thereby supporting the hypothesis that the rate of surface lowering in carbonate terrains is controlled by water convergence in the epikarst. A simple model based on the empirical correlation between denudation rate and contributing area is successful in explaining the form of several solution dolines located close to the analyzed doline. The model reveals that these solution dolines, which have varying diameters, developed over similar time scales of the order of 105 yr. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.