Correction to “Bringing the Submarine Mariana Arc and Backarc Basin to Life for Undergraduates and the Public”

IF 1 4区地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY

Island Arc Pub Date : 2024-10-17 DOI:10.1111/iar.12538

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引用次数: 0

Abstract

Stern, R. J. 2024. “Bringing the Submarine Mariana Arc and Backarc Basin to Life for Undergraduates and the Public.” Island Arc 33, no. 1: e12533. https://doi.org/10.1111/iar.12533.

Figures 3 and 4 captions should have been switched as shown below.

FIGURE 3(A) Front of a typical remotely operated vehicle (ROV). Note locations of key features: Lights, cameras (both still and video), manipulator arms, and sample baskets. Modified from NOAA ROV factsheet https://oceanexplorer.noaa.gov/edu/materials/rov-fact-sheet.pdf. (B) A typical ROV control room, from https://schmidtocean.org/cruise-log-post/technology-at-the-seafloor/.

FIGURE 4Schematic section through the upper 140 km of the Mariana convergent margen and subduction zone, showing the principal crustal and upper mantle components and their interactions. Note that the location of the “mantle wedge” (unlabeled) is that part of the mantle beneath the overriding plate and between the trench and the most distal part of the arc where subduction-related igneous or fluid activity is found. Modified after Stern (2002). MF, magmatic front.

We apologize for this error.

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更正 "让本科生和公众了解马里亚纳海底弧和后弧盆地"

Stern, R. J. 2024."Bringing the Submarine Mariana Arc and Backarc Basin to Life for Undergraduates and the Public." Island Arc 33, no 1: e12533.Island Arc 33, no. 1: e12533. https://doi.org/10.1111/iar.12533.Figures 3 和 4 的标题应如下所示对调。图 3(A) 典型遥控潜水器（ROV）的正面。注意主要特征的位置：照明灯、照相机（静态和视频）、操纵臂和样本篮。修改自 NOAA ROV 资料手册 https://oceanexplorer.noaa.gov/edu/materials/rov-fact-sheet.pdf。(B) 典型的 ROV 控制室，摘自 https://schmidtocean.org/cruise-log-post/technology-at-the-seafloor/.FIGURE 4马里亚纳汇聚边缘和俯冲带上部 140 公里的示意剖面图，显示主要的地壳和上地幔成分及其相互作用。请注意，"地幔楔"（未标注）的位置是地幔在覆载板块下方、海沟与弧的最远部分之间的部分，在那里发现了与俯冲有关的火成岩或流体活动。根据 Stern（2002 年）修改。MF，岩浆前沿。我们对这一错误表示歉意。

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来源期刊

Island Arc 地学-地球科学综合

CiteScore

2.90

自引率

26.70%

发文量

审稿时长

>12 weeks

期刊介绍： Island Arc is the official journal of the Geological Society of Japan. This journal focuses on the structure, dynamics and evolution of convergent plate boundaries, including trenches, volcanic arcs, subducting plates, and both accretionary and collisional orogens in modern and ancient settings. The Journal also opens to other key geological processes and features of broad interest such as oceanic basins, mid-ocean ridges, hot spots, continental cratons, and their surfaces and roots. Papers that discuss the interaction between solid earth, atmosphere, and bodies of water are also welcome. Articles of immediate importance to other researchers, either by virtue of their new data, results or ideas are given priority publication. Island Arc publishes peer-reviewed articles and reviews. Original scientific articles, of a maximum length of 15 printed pages, are published promptly with a standard publication time from submission of 3 months. All articles are peer reviewed by at least two research experts in the field of the submitted paper.