摘要
Yanchang Formation sited in the southern-eastern Ordos Basin has been proven a prolific reservoir unit for hydrocarbon resources. By analyzing the petrophysic data from thin-section samples, BSE, Energy Spectrum Analysis and core plugs, the authors reached the following conclusions: 1) the rimming of chlorite has an important control on the reservoir quality-such diagenetic process is characterized as a product of delta front depositional environment where is mineralogically rich in black mica and feldspar; 2) it effectively reduced the compaction effect from the overburden through burial history; 3) the associate presence of calcite re-orientated the grains into porphyroblastic structure, but arbitrarily distributed due to the small quantity; and 4) authquartz has a prominent vertical change, which is often observed as small crystal forming with chlorite rimming in a close space