Fracture development and hydrocarbon accumulation in tight sandstone reservoirs of the Paleogene Huagang Formation in the central reversal tectonic belt of the Xihu Sag, East China Sea |
ZHOU Xinhuai,XU Guosheng,CUI Hengyuan,ZHANG Wu |
Fig. 2 Typical core fracture types in the Huagang Formation. (A) Well A-2, 3619.25-3619.30 m, interlayer fractures; (b) Well B-1, 3866.50-3866.56 m, shrinkage fractures; (c) Well E-1, 4649.07-4649.74 m, tectonic fractures; (d) Well B-2, 4247.85-4248.30 m, tectonic fractures. |