Petroleum Geology

Petroleum Geology Basics

Where oil and gas come from and why they collect where they do — source rock, migration, reservoir rock, traps, and the difference between conventional and shale resources.

Oil and gas don't sit in underground lakes — they're held in the pores of rock. A working accumulation needs a complete petroleum system: a source rock that generated the hydrocarbons, a path for them to migrate, a porous reservoir rock to hold them, and a trap and seal to keep them from escaping.

This guide explains each element, plus the porosity and permeability that make a reservoir produce — and why unconventional shale plays break the classic rules.

In this guide

OpsFlo
OpsFlo for oilfield service companies.

Built by the team behind OpsFlo — field service & billing software for oilfield service companies. Capture tickets at the wellsite and bill in days, not weeks.

See OpsFlo →

Frequently asked

A source rock is an organic-rich sedimentary rock, usually marine shale, that contains kerogen — the buried remains of plankton and algae. With enough heat and burial, the kerogen matures into oil and gas.

Porosity is the percentage of void space in a rock that can hold fluids; permeability is how well those pores connect so fluid can flow. A good reservoir needs both — high porosity to store hydrocarbons and high permeability to produce them.

In conventional reservoirs, oil and gas migrated out of the source rock into a permeable trap. In unconventional (shale/tight) reservoirs, the hydrocarbons remain locked in the very low-permeability source rock itself, so they only flow economically with horizontal drilling and hydraulic fracturing.