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Interstratal dewatering origin for polygonal patterns of sand‐filled cracks: a case study from late Proterozoic metasediments of Islay, Scotland
Author(s) -
Tanner
Publication year - 1998
Publication title -
sedimentology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.494
H-Index - 108
eISSN - 1365-3091
pISSN - 0037-0746
DOI - 10.1046/j.1365-3091.1998.00135.x
Subject(s) - geology , bedding , dewatering , compaction , bed , geotechnical engineering , geomorphology , geochemistry , anisotropy , physics , quantum mechanics , horticulture , biology
Sand‐filled cracks from the Lower Fine‐grained Quartzite of Dalradian (late Proterozoic) age on the Island of Islay, western Scotland, may be divided into two main types, both of which form orthogonal and non‐orthogonal closed patterns on bedding surfaces. Type 1 cracks are short and lenticular in cross‐section, contain sand which had been injected downwards , and are found on the bottoms of cross‐laminated sandstone beds. Type 2 cracks cut several beds and preserve evidence of upward flow of water‐saturated sand. Both types of crack developed through the interstratal intrusion of water‐saturated sand into shrinkage cracks in mud or muddy sand, not, as previously thought, as a result of sub‐aerial desiccation, or sub‐aqueous cracking of the sediment surface (synaeresis). These cracks likely resulted from layer‐parallel contraction caused by compaction of mudstone layers during burial. Seismic shock may have provided the trigger for the preferential development of polygonal crack patterns in these layers instead of the more usual small‐scale dewatering structures. From a detailed comparison with published descriptions of filled cracks from a number of different geological environments, it is concluded that interstratal cracking is a mechanism which rivals sub‐aerial desiccation in importance, and is more common in the geological record than is currently realized.