What Environment are Sedimentary Rocks Formed?

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Presentation transcript:

What Environment are Sedimentary Rocks Formed?

Types of Sedimentary Rocks Introduction Origin of sedimentary rocks – Clastic Rocks – Crystalline (Chemical) and Bioclastic Sedimentary Rocks Interpreting Sedimentary Rocks – Environment of deposition – Sedimentary structures What is a Sedimentary Basin? – A thick accumulation of sediment – Necessary conditions: 1. A depression (subsidence) 2. Sediment Supply

World Map of Sedimentary Rocks Basins

Planet Earth: Liquid Water and Plate Tectonics SEDIMENTS Unconsolidated products of Weathering & Erosion – Loose sand, gravel, silt, mud, etc. – Transported by rivers, wind, glaciers, currents, etc. • Sedimentary Rock: – Consolidated sediment – Lithified sediment

Types of Sedimentary Rocks and Environment of Formation Land Derived Materials Transported by a River 3 Basic Types of Sedimentary Rocks • Land Derived ( Clastic) – Made of Rock Fragments • Crystalline (Chemical) – Precipitated from Chemical Solution • Bioclastic – Formed by remains of plants and animals

Processes of formation 1. Weathering – mechanical & chemical 2. Transport – by river, wind, glacier, ocean, etc. 3. Deposition – in a point bar, moraine, beach, ocean basin,etc 4. Lithification – loose sediment turns to solid rock

Processes during Transport • 1. Sorting – Grain size is related to energy of transport – Boulders high energy environment – Mud low energy

Stream Deposition Black shales → Source rocks Porous Sandstone Significance for Petroleum System? Black shales → Source rocks Porous Sandstone

Processes during Transport 2. Rounding – abrasion is progressive – angular grains near source – rounded grains long transport

Sorting and Rounding Bimodal rounding Poorly sorted Lithic sandstone Well rounded Well sorted Quartz sandstone Bimodal rounding Poorly sorted Lithic sandstone

Lithification • Decrease in pore space • Compaction • Decrease in pore space • Due to increasing pressure with burial • Cementation • Pores filled • quartz or calcite cements • Recrystallization • No porosity left • Beginning of metamorphism

Lithification Determines the nature of the reservoir • Critical for economic viability • Highly variable • Hard to predict ahead of the drill