The organic reef and bank facies, widely developed in Middle Ordovician Yijianfang Formation in Tahe oilfield , are characterized by point reefs and banks within the caronate platforms, and the reservoir spaces are mainly of microfissures and secondary dissolution pores.

Features of organic reefs in the Upper Permian Changxing Formation and prediction of hidden reefs in the Huanglongchang structure, eastern Sichuan;

Re-discussion of relationship between reef and giant oil-gas fields;

Late Paleozoic reefs from sequence framework in Youjiang basin;

Haline lacustrine biohermal reservoir characters in Block Da 81-4 of the Yidong Oil Field, East China;

Geology characteristics of the biohermal reservoir in Shangdian Oilfield;

Seismic exploration technology of Permian biohermal reservoir in eastern Sichuan area;

Main features of the Permian reefs of world and their palaeogeographic distribution;

Biocoenose community analysis of Bianping reefs of the Late Carboniferous in southern Guizhou Province;

Characteristics of the Permian reefs in Aergeshan,eastern Kunlun Mountains and their palaeogeographic and palaeoclimatic significance;

Diagenesis of the Upper Permian Panlongdong organic reefs in northeastern Sichuan;

The organic reefs and their reef-forming model for the Upper Permian Changxing Formation in northeastern Sichuan;

The planar distribution and significance of the organic reefs in the Lower Cretaceous Nangshan Formation in the Coqen Basin, Xizang;