An introduction-to-seismology-earthquakes-and-earth-structure-stein-and-wysession-blackwell-2003
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Primary sedimentary structures
Primary sedimentary structures are features formed during deposition of sedimentary rocks that provide information about the depositional environment. Some key primary sedimentary structures mentioned in the document include stratification, cross-bedding, ripples, graded bedding, sole marks, fossils, rip-up clasts, rainprints, desiccation cracks, imbrication, flute casts, soft-sediment deformation structures like slump folds, flame structures and clastic dikes. These structures can be used to determine paleocurrent direction, relative age, top vs bottom of strata, and the environmental conditions during deposition.
Paleogeography and Systems Tracts
Sedimentology examines sediment and rock formations on various scales, from individual grains to global patterns. It analyzes features from single clasts to depositional systems to entire basins. Sequence stratigraphy classifies rock layers into systems tracts based on their relationship to sea level changes, including falling-stage, lowstand, transgressive, and highstand tracts. It reconstructs paleogeography by correlating data from different locations and uses systems tracts to distinguish the impact of depositional events.
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Geological Structures
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aeolian landforms
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This document summarizes the Archean crustal building process. It describes how early Archean crust formed from successive volcanic eruptions that deposited greenstone belts in synclinorial basins. As the greenstone belts thickened due to continued volcanic activity and accretion, melting produced tonalite-trondhjemite-granodiorite (TTG) batholiths. Further thickening led to emplacement of potash-rich granites and the process of charnockitization around 2.6 billion years ago. The Archean crust evolved through alternating sequences of greenstone belt formation, TTG emergence, and granite intrusion driven by volcanism, melting, and mantle degassing over time.
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Lineation and foliation
Lineation refers to any linear structure that occurs repetitively in rock, such as elongated pebbles or the intersection of two foliations. Lineations can indicate the direction of tectonic transport, though opinions differ on whether they are parallel or perpendicular to transport. Foliation refers to repetitive layering in metamorphic rocks caused by shearing forces or pressure differences. Types of foliation include fracture cleavage, crenulation cleavage, slaty cleavage, and schistosity. Lineations and foliations provide important clues about a rock's deformation history.
Orogeny
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Geological structures form in the Earth's crust due to geological causes. There are many types of structures including folds, faults, and joints. Folds form when rock layers bend under stress rather than breaking. Common fold types include anticlines, synclines, domes, and basins. Faults form when rock layers fracture and move relative to each other, and include normal, reverse, and strike-slip faults. Joints are fractures where the rock splits but there is no relative movement, and can form due to processes like cooling, tectonics, and unloading.
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This document summarizes the Archean crustal building process. It describes how early Archean crust formed from successive volcanic eruptions that deposited greenstone belts in synclinorial basins. As the greenstone belts thickened due to continued volcanic activity and accretion, melting produced tonalite-trondhjemite-granodiorite (TTG) batholiths. Further thickening led to emplacement of potash-rich granites and the process of charnockitization around 2.6 billion years ago. The Archean crust evolved through alternating sequences of greenstone belt formation, TTG emergence, and granite intrusion driven by volcanism, melting, and mantle degassing over time.
Sequence stratigraphy
This document provides an outline for a course on sequence stratigraphy. It covers key concepts in stratigraphy including sedimentary depositional environments, facies analysis, sequence stratigraphy principles, and causes of sea level change. Common siliciclastic and carbonate stratigraphic successions are examined. The role of base level and relative sea level changes in controlling sediment accumulation and sequence boundaries is discussed.
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This document discusses the concept of isostasy, which refers to the equilibrium between the continental and oceanic crust due to gravitational forces. It was first defined in 1889 by American geologist Clarence Dutton. The main points are that the continental crust must be composed of lighter materials than the ocean floor to remain in equilibrium. Also, wherever the continental crust is thinner under the oceans, it extends below the ocean floor to maintain equilibrium. Early evidence for isostasy came from Pierre Bouguer's 1735 expedition to the Andes mountains, where he observed smaller than expected gravitational attraction that indicated compensation of the mountains' mass.
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Mount Everest is the highest peak on Earth at 29,028 feet above sea level.
The rock at the top of the peak is a marine limestone, deposited on the sea floor about 450
million years ago! This is an amazing fact that begs the question - how did that rock get there?
In this we will try to answer that question. The topics we will cover include:
Review of Stress and Strain
Brittle Deformation – Faults and Joints
Ductile deformation – Folds
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Stress is a force applied over an
area and therefore has units of Force/area (like lb/in 2 ). Pressure is a stress where the forces act
equally from all directions.
If stress is not equal from all
directions then we say that
the stress is a differential
stress. Three kinds of
differential stress occur.
1. Tensional stress (or
extensional stress),
which stretches rock;
2. Compressional stress,
which squeezes rock;
and
3. Shear stress, which
result in slippage and
translation
When rocks deform they are said to strain. A strain is a change in size, shape, or volume of a
material. We here modify that definition somewhat to say that a strain also includes any kind of
movement of the material, including translation and tilting.
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is a form of mass wasting that includes a wide range of ground movements, such as rockfalls, deep failure of slopes, and shallow debris flows. Landslides can occur underwater, called a submarine landslide, coastal and onshore environments. Although the action of gravity is the primary driving force for a landslide to occur, there are other contributing factors affecting the original slope stability. Typically, pre-conditional factors build up specific sub-surface conditions that make the slope area prone to failure, whereas the actual landslide often requires a trigger before being released. Landslides should not be confused with mudflows, a form of mass wasting involving very to extremely rapid flow of debris that has become partially or fully liquefied by the addition of significant amounts of water to the source material.
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Mount Everest is the highest peak on Earth at 29,028 feet above sea level.
The rock at the top of the peak is a marine limestone, deposited on the sea floor about 450
million years ago! This is an amazing fact that begs the question - how did that rock get there?
In this we will try to answer that question. The topics we will cover include:
Review of Stress and Strain
Brittle Deformation – Faults and Joints
Ductile deformation – Folds
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Stress is a force applied over an
area and therefore has units of Force/area (like lb/in 2 ). Pressure is a stress where the forces act
equally from all directions.
If stress is not equal from all
directions then we say that
the stress is a differential
stress. Three kinds of
differential stress occur.
1. Tensional stress (or
extensional stress),
which stretches rock;
2. Compressional stress,
which squeezes rock;
and
3. Shear stress, which
result in slippage and
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https://www.linkedin.com/in/saif-abo-khashaba-237915148/
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1. Saltation occurs when loose material is lifted from the bed surface by wind or water and travels in ballistic trajectories before settling back onto the surface.
2. Traction involves the rolling or sliding of sand grains and larger clasts along the bed as they interact with the substrate.
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The document discusses the geological concept of isostasy. Isostasy refers to the principle of buoyancy where land masses float on the denser underlying mantle material. It explains that mountains create indentations in the earth's crust similar to placing a heavy object on a rubber ball. It also describes early theories on isostasy from Clarence Dutton, who coined the term, and Sir George Airy, who proposed that land masses float with varying thickness but uniform density. The concept was later refined by A. Pratt to propose uniform depth but varying density between land masses.
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Wind / Aeolian landforms
The document discusses various landforms created by wind erosion including deflation basins, mushroom rocks, yardangs, and ventifacts. It describes the three main types of wind erosion: attrition, deflation, and abrasion. Additionally, it examines the transportational and depositional work of wind, which forms features such as sand dunes, ripple marks, and loess deposits.
Fault'classification of fault and mechanism of faulting
This document summarizes a seminar on faults presented by Aditi Jena to her professor. It defines a fault as a fracture in rock across which there is significant displacement. Faults are classified based on their dip, pattern of movement, and stress conditions. The main types are normal faults which form during tension, reverse/thrust faults during compression, and strike-slip faults when the intermediate stress axis is vertical. Fault planes develop at 30 degrees to the maximum stress and slip occurs perpendicular to the intermediate stress. Examples like the San Andreas fault and Main Central Thrust are given to illustrate different fault types.
Mississippi valley type deposits
This document discusses Mississippi Valley-type (MVT) deposits, which are important sources of lead and zinc found hosted in carbonate rocks. MVT deposits form from hydrothermal fluids emanating from deep shale source rocks that are overpressured. These fluids flow upward through aquifers, depositing zinc, lead, and sometimes fluorite minerals in fractures or pores in carbonate host rocks. MVT deposits are classified into zinc-dominant, lead-dominant, and fluorite-dominant subtypes based on primary mineral associations. Factors influencing MVT deposit formation include porosity in the host rock and sufficient quantities of trace elements in migrating fluids. Examples of MVT deposits in Pakistan include occurrences in Jurassic
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The document discusses the classification of folds based on various parameters such as fold closure, symmetry, plunge, orientation of the axial plane, and nature of the hinge line. Folds are classified into different types including antiform, synform, symmetrical, asymmetrical, horizontal, plunging, upright, recumbent, and overturned folds based on these parameters. The classification schemes proposed by Fluety (1964) and Ramsay (1967) are also summarized.
Geosyncline
The document discusses the concept of geosynclines, which refers to thick piles of sediments deposited in deep marine basins that were later compressed, deformed, and uplifted to form mountain ranges. Geosynclines developed in three phases - first sediments accumulated in a subsiding trough (geosynclinal phase), then the deeply buried sediments folded under heat and pressure (tectonic phase), and finally horizontal compression forces uplifted the folded rocks to form mountains tens of thousands of meters high (orogenic phase). Geosynclines are classified as orthgeosynclines like eugeosynclines that formed far from continents with volcanic rocks, or parageosynclines like miogeosyn
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This document defines and describes different types of unconformities in geology. It begins by defining an unconformity as a break or gap in the geological record representing a period of erosion or non-deposition. It then describes the major types of unconformities, including angular, disconformity, non-conformity, and local unconformities. Finally, it outlines several ways that unconformities provide significance, such as indicating time intervals missing from the geological record, structural discordances between rock layers, evidence of past topography, and signs of weathering at the contact surface.
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Tectonites are deformed rocks whose fabric is due to systematic movement under external forces. Their fabric reflects the deformation history. Fabric includes the geometric arrangement of mineral grains, layers, and other features at a scale that includes many samples. Tectonites can have planar (S-tectonite), linear (L-tectonite), or both (L-S tectonite) fabrics indicating different strain types. Foliations like cleavage, schistosity, and gneissosity are planar fabrics that cause rocks to break along parallel surfaces. Lineations indicate preferred linear fabrics, such as fold axes, boudins, and quartz rods. The orientation and interaction of foliations and lineations provide information about tect
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- More damage occurs closer to the epicenter where the seismic waves are strongest. The Richter scale, seismographs, and other keywords are defined and linked to understanding earthquakes.
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This lecture discusses introductory mechanics models and constitutive models for biomaterials. The objectives are to establish biomaterial constitutive models, determine biomechanical response to load, analyze prosthetic design, and estimate health status of living tissues under stress. The lecture covers introductory mechanics modeling including stress analysis, normal and pure bending. Methods of biomechanics including analytical, experimental, and numerical techniques like FEM are presented. Constitutive models including elastic behavior, Hooke's law, elastic constants, material anisotropy, orthotropy, transverse isotropy, and isotropy are discussed.
Richter scale and mercalli scale
The document summarizes the Richter and Mercalli scales used to measure earthquake magnitudes. The Mercalli scale uses qualitative descriptions of earthquake effects on people and structures, while the Richter scale provides quantitative measurements of seismic wave amplitude. The Richter scale is logarithmic, with each whole number step representing a tenfold increase in measured amplitude. It allows for easier comparison of earthquake magnitudes regardless of location.
Earth Science 6.2 : Effects of Volcanic Eruptions
Volcanic eruptions can profoundly impact climate and the Earth's surface. Large eruptions eject ash and gases into the atmosphere, which can block sunlight and cause global temperatures to drop. There are three main types of volcanoes: shield volcanoes formed from nonexplosive eruptions creating gentle slopes; cinder cone volcanoes from moderately explosive eruptions forming steep slopes; and composite volcanoes from alternating explosive and lava flows creating broad bases that steepen toward their summits. In addition to volcanoes, other volcanic landforms include craters at volcano tops, calderas which are large depressions formed when the magma chamber empties, and lava plateaus resulting from nonexplosive eruptions
Basic well log analysis for geologist george asquith, aapg
Basic well log analysis from Asquith, early book that provide a good interpretation in petrophysic/formation evaluation.
Earth Science 5.2 : Earthquake Measurement
Seismographs are used to detect earthquakes and locate their epicenters. Scientists use seismograms from multiple seismographs to determine the time an earthquake's waves arrived using the S-P Time Method, locating the epicenter above the focus where it began. The Richter scale measures an earthquake's magnitude based on the ground motion recorded, adjusted for distance to the seismograph. The Modified Mercalli Intensity Scale further describes earthquake impacts from I (not felt) to XII (total damage), with higher intensities nearer the epicenter.
Richter Scale 1 To 10
The document describes the Richter Scale, which measures the strength of earthquakes. The scale ranges from 0 to 10, with 0 representing a light earthquake and 10 representing a mega earthquake, the most extreme type of earthquake on the scale. Earthquakes between 3-6 are considered moderate to severe, while those over 7 are very extreme to highextreme, the most powerful earthquakes.
Earth Science 6.1 : Volcanic Eruptions
This document discusses volcanic eruptions, describing the differences between nonexplosive and explosive eruptions. Nonexplosive eruptions produce slow lava flows while explosive eruptions blast debris into the air. The type of eruption depends on the composition of the magma, particularly its silica, water, and gas content. Magma erupts as either lava or pyroclastic material like volcanic ash, bombs, and blocks.
Seismic refraction method lecture 21
Seismic refraction is a method that uses seismic waves, specifically P-waves, to investigate geological structures below the Earth's surface. There are two main types of elastic body waves: P-waves and S-waves. P-waves travel faster and are studied in simple seismic methods. When seismic waves encounter an interface between geological layers, the waves are reflected, refracted, and converted between P and S-waves. Refraction occurs when the velocity increases with depth, causing head waves that travel parallel to interfaces and are recorded by geophones on the surface. Snell's law governs refraction and describes how the refraction angle changes based on the velocity in each layer.
Seismic Waves
Seismic waves are waves of energy caused by the sudden breaking of rock within the Earth or explosions. There are two main types of seismic waves: body waves and surface waves. Body waves include P waves and S waves, which travel through the Earth's interior. Surface waves such as Love waves and Rayleigh waves travel along the Earth's surface and cause the most shaking during an earthquake. Seismic waves are recorded by seismographs and can provide information about the Earth's interior structure.
Seismic Reflection
Seismic Reflection presented to master students in Geotechnical and Earthquake Engineering in Civil Engineering Department_EMU
Well logging
Well logging involves lowering instruments into boreholes to record measurements of the surrounding geological formations. There are two main types: geological logs based on visual inspection of cuttings or cores brought to the surface, and geophysical logs using downhole instruments to measure physical properties like resistivity, acoustic properties, and radioactivity. Well logging is used for oil and gas exploration and production as well as other purposes like groundwater and environmental studies. It provides important information about parameters like porosity, permeability, and fluid content of the formations.
well logging project report_ongc project student
This dissertation report discusses characterizing oil and gas reservoirs using open hole wireline logging tools and techniques. It provides background on reservoir properties that can be measured using logs like resistivity, porosity, and saturation. It also describes the various electrical, radioactive, sonic, and other open hole wireline logging tools and their measurement principles.
Well logging
This document discusses borehole geophysical logging and resistivity logging. It describes:
1. The objectives of borehole logging including characterizing the borehole environment, invasion depth and profile.
2. Conditions that affect the borehole such as hole size, drilling mud, mud cake and filtrate.
3. How resistivity logs work by measuring the resistivity of formations and fluids to determine lithology, fluid content and invasion.
4. Types of resistivity logging tools like lateral logs and micro-resistivity tools and how they make measurements in the flushed, transition and undisturbed zones.
Basic well logging design
The document discusses the basics of well logging design. It includes an agenda for a one-day course that covers basic logging theory, interpretation, logging program design, and a workshop. The objectives are to familiarize participants with various log measurements, well evaluation strategies, and approaches to well logging design. Key logging topics covered include definitions, history, measurement principles for resistivity, spontaneous potential, gamma ray, density, neutron, and acoustic logs. Interpretation applications and limitations are also discussed.
Earth's magnetism
The document discusses the dynamo theory of the Earth's magnetism. It proposes that electric currents produced by the movement of liquid iron in the Earth's outer core generate the planet's magnetic field. Convection currents provide the energy needed to sustain the magnetic field over geological timescales. Paleomagnetic studies of fossil magnetism in rocks support the idea that the Earth's magnetic poles have reversed polarity multiple times in the past, consistent with the dynamo theory.
Geophysical well logging
Geophysical well logging uses sensors located in boreholes to measure physical properties of surrounding rocks as a function of depth. Well logs are used to identify geological formations and fluids, correlate between holes, and evaluate reservoir formations. Common logging methods include electrical resistivity, self-potential, nuclear, acoustic, and thermal measurements. The objective is to determine in situ rock and fluid properties, though drilling disturbs the formation. Effective depth of penetration varies between tools and formations. Well logging aims to identify potential reservoirs by determining porosity, permeability, and fluid contents.
Permeabilidad en rocas
Este documento trata sobre la mecánica de suelos y rocas. Explica conceptos como la permeabilidad, porosidad y factores que afectan la velocidad de flujo en los suelos. Define la permeabilidad como la capacidad de un material para permitir el paso de un fluido a través de sus poros sin alterar su estructura interna. También describe los diferentes tipos de poros en los suelos y cómo afectan su comportamiento con respecto al agua y aire. Finalmente, clasifica los suelos en permeables e impermeables y explica
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