Dolomite can form as a major mineral component of marlstones and limestones and is an
important sink for magnesium in the marine environment. Dolomite is widely distributed in …

In structurally-controlled dolomitization systems, there is a general consensus that the
formation of dolostone-limestone transitions, termed here as “dolomitization fronts”, is …

Cores, thin sections, and cathodoluminescence analysis were integrated to document the
occurrence and petrology of dolomites, and their pore systems in the Cambrian of Tarim …

The complex tectonic activities and multi-stage diagenetic modifications lead to the
formation of a heterogeneous pore network spectrum ranging from macropores (centimeter …

为揭示深层碳酸盐岩储层的成因机理, 对塔里木盆地顺南地区蓬1 井进行了研究. 顺南蓬1
井取心段揭示, 在埋深超过7 500 m 的碳酸盐岩中发育有大量的裂缝和溶蚀孔洞 …

Dolomite reservoirs formed by dissolution are significant for hydrocarbon exploration, but
their origins are poorly understood because of their complexity. This study investigated the …

Thermal convection arises due to a density gradient between geothermally heated formation
water within the underlying strata and the water in the overlying strata. The thermal …

The present study investigates the microfacies and the effects of diagenetic processes on
the reservoir quality of limestones of the Fort Member, Jaisalmer Formation, Western …

Abstract The deeply buried (> 7 km) upper Ediacaran (Sinian) Dengying Formation (ca.
551.1–541 Ma) in the Sichuan Basin, China, is the largest Precambrian dolostone gas …

Abstract The Meillon (Callovo-Oxfordian) and Mano (Tithonian) Formations are dolomitized
carbonate reservoirs that actively produce oil and gas (Aquitaine Basin, France). In this …