Abstract
Yang et al., Acta Geologica Sinica-English Edition, 91(2), pp. 749–750 claim that they discovered supercritical hyperpycnal flow deposits in the Early Cretaceous strata on Lingshan Island, East China. We would like to discuss this paper under the following topics: (a) the terminology of “supercritical hyperpycnal flow,” (b) hyperpycnal flow deposition, and (c) supercritical flow deposition. Our aim is twofold in that the following debate will help unravel the complexities associated with the controversy around the paleosedimentary environment and sediment dynamic processes of the early Cretaceous deposits on Lingshan Island, in addition to providing an understanding of hyperpycnal flow and supercritical flow deposits. The Beilaishi section deposits on Lingshan Island are more likely storm-induced tempestites within the lacustrine basin delta front and associated deep lacustrine turbidites. Frequent earthquakes due to tectonic-magmatic activity are the most likely triggers for lacustrine storms.
Original language | English |
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Pages (from-to) | 5508-5513 |
Number of pages | 6 |
Journal | Geological Journal |
Volume | 55 |
Issue number | 7 |
Early online date | 27 Jan 2020 |
DOIs | |
Publication status | Published - Jul 2020 |
Bibliographical note
Funding information: China‐ASEAN Maritime Cooperation Fund Project, Grant/Award Number: 12120100500017001; Northeast Petroleum University Scientific Research Start‐up Fund; Youth Foundation of Northeast Petroleum University, Grant/Award Number: NEPUBS201503; Scientific and Technological Innovation Project of Qingdao National Laboratory for Marine Science and Technology, Grant/Award Number: QNLM201708; Natural Science Foundation of Shandong Province, Grant/Award Number: ZR2016DB15; Natural Science Foundation of Heilongjiang Province, Grant/Award Number: JJ2016ZR0573Keywords
- Early Cretaceous
- hyperpycnal flow
- Lingshan Island
- supercritical flow
- tempestites
- HUMMOCKY CROSS-STRATIFICATION
- SEDIMENT DEFORMATION STRUCTURES
- RECOGNITION
- TEMPESTITE
- SANDSTONES
- FACIES
- GRADED TURBIDITE SEQUENCES
- CYCLIC STEPS
- BASIN
- DEEP-WATER