Types and origin of dolostones in the Lower Palaeozoic of the North China Platform

Abstract

Dolostones are very common in the Lower Palaeozoic of the North China Platform. They can be divided into two large groups: mud-silt-sized crystalline dolostones and saccharoid dolostones. The former can be further divided into gypsiferous and nongypsiferous mud-silt-sized crystalline dolostones and the latter into equal-sized and unequal-sized saccharoid dolostones. Gypsiferous, mud-silt-sized, crystalline dolostones are well laminated, show bird's-eyes and mudcracks, and contain gypsum crystals or nodules. Their δ 13C is +0.42‰ to +2.21‰, and δ 18O is −6.01‰ to −4.77‰ (PDB standard). These dolostones are similar sedimentologically to the sabkha penecontemporaneous dolostones in the Persian Gulf and were formed in supratidal flats by hypersaline sea water in arid conditions. Nongypsiferous, mud-silt-sized, crystalline dolostones are similar to the gypsiferous ones in texture and structure but do not contain gypsum. Their δ 13C is −3.69‰ to +3.41‰, and δ 18O is −8.17‰ to −4.04‰. They are similar to the supratidal penecontemporaneous dolostones on the Bahamian Platform and were formed in supratidal flats by hypersaline sea water in humid conditions. Equal-sized saccharoid dolostones are composed of dolomites of approximately the same size. Their δ 13C is −2.11‰ to +2.10‰, and δ 18O is −9.33‰ to −4.09‰. These dolostones mainly resulted from dorag dolomitization. Unequal-sized saccharoid dolostones are composed of dolomites of greatly different sizes. Their δ 13C is −4.72 to −1.08, and δ 18O is −9.27‰ to −7.32‰ . These dolostones resulted from the recrystallization of earlier dolostones. The reservoir characteristics of dolostones are affected by many factors. Production practice shows that non-clayey silt-sized crystalline dolostones are the best dolostone reservoir rocks.