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Particuology 2014年第2期12卷 150-150页

作者： David Y.H.Pui Junji Cao Zhisheng An Jing Wang

We are grateful for the experts＇ comments on our manuscript. We fully understand the experts＇ concerns on the feasibility of the proposed idea of building windbreak walls equipped with solar panels to mitigate the yellow dust storm. As stated in the manuscript, we have not considered many important factors, such as the limits posed by solar panels, operability of solar panels under harsh conditions, the local weather and geomorphological conditions, electricity storage and transportation, financial aspects, etc. However, the manuscript is intended to present a Big Idea to stimulate more interesting ideas to solve Big Problems.

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reply to the comment by Tan Mingxuan et al.(2017), on “A new Discovery of the Early Cretaceous Supercritical Hyperpycnal Flow Deposits on the Lingshan Island, East China”

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Acta Geologica Sinica(English Edition) 2017年第6期91卷 2346-2348页

作者： YANG Tian CAO Yingchang WANG Yanzhong School of Geosciences China University of Petroleum (East China) Shandong Provincial Key Laboratory of Depositional Mineralization & Sedimentary Minerals Shandong University of Science and Technology Laboratory for Marine Mineral Resources Qingdao National Laboratory for Marine Science and Technology

We thank Tan Mingxuan et al. （2017） for their comments stimulated by our short paper in the recent Acta Geologica Sinica （English edition）. We are grateful for the opportunity to expand on the model of the supercritical hyperpycnal flow deposits in the Beilaishi section on the Lingshan Island, and to explain why the model proposed by Tan Mingxuan et al. （2017） cannot explain the bulk of the deposits in the Beilaishi section. We do not dispute that the recognition of supercritical flow deposits remains ambiguous （Ono and Plink-Bjorklund, 2017）. To some extent, the morphology of deep-water supercritical flow deposits is similar to hummocky and swaley cross- stratification （Ono and Plink-Bjorklund, 2017）. Besides, distinguishing the deposits laid down by gravity flows in deep-water systems from those produced by storm-related combined flows in continental shelf systems is not an easy task （Ono and Plink-Bjorklund, 2017）. However, a correct interpretation is crucial for understanding the paleogeographic and depositional model.

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