The formation of tepee-like structure in Neoproterozoic cap carbonate;

The transfer of atmospheric carbon dioxide to the ocean would result in the rapid precipitation of calcium carbonate in warm surface waters and consequently formation of the cap carbonate rocks.

As an enduring enigma of Neoproterozoic, the Cap Carbonate has been found in many regions of the world on lying on the glacial diamictites with negative carbon isotopic.

Based on the microfacies studies of the cap carbonates from the Sinian Doushantuo Formation at Jiulongwan section of Yichang, Hubei, we consider the cap carbonates are stable mud peloidal limestone and recrystallized in varying degrees after the deposition.

Inquire into Compound Oil and Gas Well Logging in Carbonate Rock of Marine Facies in Northeast Sichuan;

Study on the fractured reservoir of the carbonate rock in Sha 1 lower sub-interval in Wangxuzhuang Oilfield;

Research into the feasibility of the treatment of high-concentrated arsenic acidic coal mine wastewater by carbonate rocks;

The Characteristics and the Formation Mechanism of the Carbonate Reservoir in Jialingjiang Formation in the Southeast Area of the Southern Sichuan Basin;

High-precision seismic exploration in carbonate karst cave developed area;

A study on the structural evolution and the petroleum characteristics of Gudao carbonate buried hill in Jiyang depression,China;

Study on diagenesis of the carbonate rocks in the Carboniferous sequence stratigraphic framework of South Guizhou;

Restudy of tamer reservoir of buried hill of low-Paleozoic carbonate rocks in Jiyang Depression;

REE characteristics of carbonate rocks in Xicheng Devonian basin and origin of dolomite in Changba giant lead-zinc deposit;