Coexistence of Hyperpycnites, Debrites and Turbidites and Their Geological Significances of Unconventional Petroleum
Coexistence of Hyperpycnites, Debrites and Turbidites and Their Geological Significances of Unconventional Petroleum
复制标题
异重岩、碎屑岩、浊积岩共存及其非常规石油地质意义
DOI：
10.1111/1755-6724.12302_49
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发表时间：
2015-09
期刊：
影响因子：
--
通讯作者：
Fan Aiping
中科院分区：
文献类型：
--
作者：
Yang Renchao;Jin Zhijun;Sun Dongsheng;Han Zuozhen;Fan Aiping
深水砂岩的成因已成为沉积学研究和石油工业的焦点（Etienne等人，2012），然而，人们对这些深水沉积物流动和沉积机制仍然知之甚少（Talling et a.，2012年）。在过去的几十年里，大多数深水砂体被解释为浊流，直到新的桑迪泥石流理论挑战了经典的浊流理论（Shanmugam，1996）。更重要的是，对高密度流的新认识实现了浊流理论（Mulder等人，1995年）。尽管沉积学家对某些深水砂岩的成因仍存在争议，但桑迪泥石流、浊流和高密度流之间的关系已被一致认为是深水重力流和深水沉积学的关键科学问题。桑迪泥石流、浊流和超稠流之间不仅存在复杂的转化和诱导作用，而且超稠岩、碎屑岩和浊流在时间和空间上往往共生共存。长期地史中地质条件的多变性和复杂性决定了沉积学家对同一沉积产物存在多种解释。
The genesis of deep water sandstone has become the focus both of sedimentology research and petroleum industry (Etienne et al., 2012), however, people still know little about these deep water sediments flows and depositional mechanisms (Talling et a.,2012). Most of the deep water sandbodies were interpreted as turbidites in the past decades, until new theory of sandy debris flow challenged the classic theory of turbidity current (Shanmugam, 1996). What is more, new understanding of hyperpycnal flow fulfilled the theory of turbidity current (Mulder et al., 1995). Although arguments still exist among sedimentologists on origination of some deep water sandstone, relationships among sandy debris flows, turbidity currents and hyperpycnal flows were unanimously agreed to be the key scientific issue of deep water gravity flows and deep water sedimentology. Complex transformations and inductions not only exist among sandy debris flows, turbidity currents and hyperpycnal flows, but also hyperpycnites, debrites and turbidites co-occurs and co-exist in time and space usually. The variability and complexity of geological conditions in long geohistory determine the existence of multiple explanations of the same deposition products among sedimentologists.
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影响因子：
5.8
作者：
E. Sumner;M. Siti;L. McNeill;P. Talling;T. Henstock;R. Wynn;Y. Djajadihardja;H. Permana
通讯作者：
E. Sumner;M. Siti;L. McNeill;P. Talling;T. Henstock;R. Wynn;Y. Djajadihardja;H. Permana
影响因子：
5.8
作者：
Y. You;P. Flemings;D. Mohrig
通讯作者：
Y. You;P. Flemings;D. Mohrig
影响因子：
3.5
作者：
P. Talling;D. Masson;E. Sumner;G. Malgesini
通讯作者：
P. Talling;D. Masson;E. Sumner;G. Malgesini
影响因子：
1.8
作者：
MULDER, T;SYVITSKI, JPM
通讯作者：
SYVITSKI, JPM
影响因子：
5.8
作者：
Clare, Michael A.;Talling, Peter J.;Hunt, James
通讯作者：
Hunt, James