{"title":"更正为 \"意大利西西里岛东北部帕利亚拉盆地一个紧密耦合的源-汇系统中的综合隆升、沉降、侵蚀和沉积","authors":"","doi":"10.1111/bre.12851","DOIUrl":null,"url":null,"abstract":"<p>Pavano, F., Pazzaglia, F. J., Rittenour, T. M., Catalano, S., Corbett, L. B., & Bierman, P. (2024). Integrated uplift, subsidence, erosion and deposition in a tightly coupled source- to- sink system, Pagliara basin, northeastern Sicily, Italy. Basin Research, 36, e12845. https://doi.org/10.1111/bre.12845</p><p>In Table 4, the table note was incorrect. This should have read:</p><p>“We used 5.0E-7 yrs for the <sup>10</sup>Be decay constant and 1,386,555 yrs for the half-life. <sup>10</sup>Be exposure is modeled using the CRONUS-Earth online calculators (Balco et al., 2008) to have occurred at a mean elevation of 420 m, which we derived from the assumed steady-state hypsometry of the Pagliara basin (670 m, Pavano et al., 2016), less 250 m of post-middle 300 ka uplift of the Pagliara basin”.</p><p>The References list should include the following:</p><p>Balco, G., Stone, J. O., Lifton, N. A., and Dunai, T. J., 2008, A complete and easily accessible means of calculating surface exposure ages or erosion rates from 10Be and 26Al measurements: Quaternary Geochronology, 3, 174–195.</p><p>In Section 5.2 “Cosmogenic <sup>10</sup>Be paleo-erosion rate data” the text “The measured <sup>10</sup>Be concentrations (Nt) (Table 3) are increased to their decay-corrected burial values (No) using the <sup>10</sup>Be decay constant of 4.3 e-09 yr<sup>-1</sup>” was incorrect. This should have read “The measured <sup>10</sup>Be concentrations (Nt) (Table 3) are increased to their decay-corrected burial values (No) using the <sup>10</sup>Be decay constant of 5.0e-7 yr<sup>-1</sup>”.</p><p>We apologize for this error.</p>","PeriodicalId":8712,"journal":{"name":"Basin Research","volume":"36 1","pages":""},"PeriodicalIF":2.8000,"publicationDate":"2024-02-17","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1111/bre.12851","citationCount":"0","resultStr":"{\"title\":\"Correction to Integrated uplift, subsidence, erosion and deposition in a tightly coupled source-to-sink system, Pagliara basin, northeastern Sicily, Italy\",\"authors\":\"\",\"doi\":\"10.1111/bre.12851\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>Pavano, F., Pazzaglia, F. J., Rittenour, T. M., Catalano, S., Corbett, L. B., & Bierman, P. (2024). Integrated uplift, subsidence, erosion and deposition in a tightly coupled source- to- sink system, Pagliara basin, northeastern Sicily, Italy. Basin Research, 36, e12845. https://doi.org/10.1111/bre.12845</p><p>In Table 4, the table note was incorrect. This should have read:</p><p>“We used 5.0E-7 yrs for the <sup>10</sup>Be decay constant and 1,386,555 yrs for the half-life. <sup>10</sup>Be exposure is modeled using the CRONUS-Earth online calculators (Balco et al., 2008) to have occurred at a mean elevation of 420 m, which we derived from the assumed steady-state hypsometry of the Pagliara basin (670 m, Pavano et al., 2016), less 250 m of post-middle 300 ka uplift of the Pagliara basin”.</p><p>The References list should include the following:</p><p>Balco, G., Stone, J. O., Lifton, N. A., and Dunai, T. J., 2008, A complete and easily accessible means of calculating surface exposure ages or erosion rates from 10Be and 26Al measurements: Quaternary Geochronology, 3, 174–195.</p><p>In Section 5.2 “Cosmogenic <sup>10</sup>Be paleo-erosion rate data” the text “The measured <sup>10</sup>Be concentrations (Nt) (Table 3) are increased to their decay-corrected burial values (No) using the <sup>10</sup>Be decay constant of 4.3 e-09 yr<sup>-1</sup>” was incorrect. This should have read “The measured <sup>10</sup>Be concentrations (Nt) (Table 3) are increased to their decay-corrected burial values (No) using the <sup>10</sup>Be decay constant of 5.0e-7 yr<sup>-1</sup>”.</p><p>We apologize for this error.</p>\",\"PeriodicalId\":8712,\"journal\":{\"name\":\"Basin Research\",\"volume\":\"36 1\",\"pages\":\"\"},\"PeriodicalIF\":2.8000,\"publicationDate\":\"2024-02-17\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://onlinelibrary.wiley.com/doi/epdf/10.1111/bre.12851\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Basin Research\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://onlinelibrary.wiley.com/doi/10.1111/bre.12851\",\"RegionNum\":2,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"GEOSCIENCES, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Basin Research","FirstCategoryId":"89","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1111/bre.12851","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
引用次数: 0
摘要
Pavano, F., Pazzaglia, F. J., Rittenour, T. M., Catalano, S., Corbett, L. B., & Bierman, P. (2024).Integrated uplift, subsidence, erosion and deposition in a tightly coupled source-to-sink system, Pagliara basin, northeastern Sicily, Italy.Basin Research, 36, e12845。https://doi.org/10.1111/bre.12845In 表 4，表格注释有误。应改为："我们使用 5.0E-7 年作为 10Be 的衰变常数，使用 1,386,555 年作为半衰期。我们使用 CRONUS-Earth 在线计算器（Balco 等人，2008 年）模拟了 10Be 暴露发生在 420 米的平均海拔高度，这是我们根据假定的 Pagliara 盆地稳态湿度测量值（670 米，Pavano 等人，2016 年）得出的，减去 250 米的后海拔高度、参考文献列表应包括以下内容：Balco, G., Stone, J. O., Lifton, N. A., and Dunai, T. J., 2008, A complete and easily accessible means of calculating surface exposure ages or erosion rates from 10Be and 26Al measurement：在第 5.2 节 "宇宙成因 10Be 古侵蚀率数据 "中，"利用 10Be 衰变常数 4.3 e-09 yr-1，将测得的 10Be 浓度（Nt）（表 3）提高到衰变校正埋藏值（No）"有误。我们对这一错误表示歉意。
Correction to Integrated uplift, subsidence, erosion and deposition in a tightly coupled source-to-sink system, Pagliara basin, northeastern Sicily, Italy
Pavano, F., Pazzaglia, F. J., Rittenour, T. M., Catalano, S., Corbett, L. B., & Bierman, P. (2024). Integrated uplift, subsidence, erosion and deposition in a tightly coupled source- to- sink system, Pagliara basin, northeastern Sicily, Italy. Basin Research, 36, e12845. https://doi.org/10.1111/bre.12845
In Table 4, the table note was incorrect. This should have read:
“We used 5.0E-7 yrs for the 10Be decay constant and 1,386,555 yrs for the half-life. 10Be exposure is modeled using the CRONUS-Earth online calculators (Balco et al., 2008) to have occurred at a mean elevation of 420 m, which we derived from the assumed steady-state hypsometry of the Pagliara basin (670 m, Pavano et al., 2016), less 250 m of post-middle 300 ka uplift of the Pagliara basin”.
The References list should include the following:
Balco, G., Stone, J. O., Lifton, N. A., and Dunai, T. J., 2008, A complete and easily accessible means of calculating surface exposure ages or erosion rates from 10Be and 26Al measurements: Quaternary Geochronology, 3, 174–195.
In Section 5.2 “Cosmogenic 10Be paleo-erosion rate data” the text “The measured 10Be concentrations (Nt) (Table 3) are increased to their decay-corrected burial values (No) using the 10Be decay constant of 4.3 e-09 yr-1” was incorrect. This should have read “The measured 10Be concentrations (Nt) (Table 3) are increased to their decay-corrected burial values (No) using the 10Be decay constant of 5.0e-7 yr-1”.
期刊介绍：
Basin Research is an international journal which aims to publish original, high impact research papers on sedimentary basin systems. We view integrated, interdisciplinary research as being essential for the advancement of the subject area; therefore, we do not seek manuscripts focused purely on sedimentology, structural geology, or geophysics that have a natural home in specialist journals. Rather, we seek manuscripts that treat sedimentary basins as multi-component systems that require a multi-faceted approach to advance our understanding of their development. During deposition and subsidence we are concerned with large-scale geodynamic processes, heat flow, fluid flow, strain distribution, seismic and sequence stratigraphy, modelling, burial and inversion histories. In addition, we view the development of the source area, in terms of drainage networks, climate, erosion, denudation and sediment routing systems as vital to sedimentary basin systems. The underpinning requirement is that a contribution should be of interest to earth scientists of more than one discipline.
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