Table of Contents 1. INTRODUCTION 2 1.1. Subject and motivation for report 2 1.2. Geographic location of study area………………………...……………………………2 1.3. Objectives of report…………………………………………………………………….2 1.4. Plan of development 3 2. REGIONAL GEOLOGIC SETTING………………………………………………………….3 2.1. The main Karoo Basin………………...………………………………………………..3 3. THE TANQUA KAROO FANCOMPLEX……………………………………………………5 3.1. Sequence stratigraphic framework………………………………………………….….5 4. TURBIDOTE DEPOSITS AND HYDROCARBONEXPLORATION……………………….6 4.1. Tanqua outcrop analogue……………………………………………………………....7 4.1.1. Basin floor fan………………………………………………………………..7 4.1.2. Proximal fan…………………………………………………………………..7 4.1.3. Transition from proximal to medial fan………………………………………8 4.1.4. Medial fan…………………………………………………………………….8 4.1.5. Distal fan……………………………………………………………..……….8 4.2. …show more content…
It aims to provide insight into the geological as well as petrophysical complexity of existing deep-water turbidite reservoirs, the flow of hydrocarbons through them, and the best ways of developing them. To serve this purpose the Diana field, western Gulf of Mexico, is assessed with analogous reservoir characteristics of the turbidites of the Tanqua Fan Complex (Fig.5). The Diana field is located on the western Gulf of Mexico and it lies 260km south of Galieston in approximately 1430 metres of water (Sullivan et al., 2004). The reservoir rocks comprise of turbiditic sandstones, similar to those of the Tanqua Fan Complex. Despite the fact that the field is known to have recoverable hydrocarbons in excess of 100 MMBOE (Sullivan et al., 2004), there are too many uncertainties regarding flow simulation and well-performance prediction. The main challenges are; • Variable-quality seismic data • Reservoir thickness expressed by a single cycle event • Likelihood of sub-seismic
The rocks do not show signs of heavy weathering. There is some white staining visible, but there is very little red or brown staining. The rocks have abundant vesicles. There is a mix of rocks with varying sizes and numbers of vesicles. Samples collected were representative of this mix.
The article states three competting theories about Chano Canyon and provides three theories. However, the professor explains that these theories are not correct and refutes each of the author 's reasons. First, the reading claims that the Chaco structure were purely residental, with each housing handred of people. The professor refutes this point by saying that this theiry can not be correct.
The fossils which can be observed include brachiopods and rugose corals. Specific species of corals have been identified in Bellapenna’s report since they are the most widespread fossil within the Cordell dolostone. The interbedded chert can be observed in the field. The gradation of gray to blue to brown chert nodules can also be observed. Bellapenna also suggests there are quartz and garnet grains within the Dolostone.
The construction of the Kinzua Dam in the 1960 has been symbolic to the Seneca Nation people. Ohi:yo dwagahdegyo:’ -I am from the ancestral land that covered 10,000 acres that ran along the ohi:yo; Alleghany River. In 1794 Seneca nation signed a peace treaty with the United States that guaranteed land for the Seneca people. Article three in the 1794 treaty declared that “the United States acknowledge all the land within the aforementioned boundaries, to be the property of the Seneka [sic] nation; and the United States will never claim the same, nor disturb the Seneka nation.” The inception of Kinzua Dam initiated in 1950 while the Seneca nation people were unaware.
Summary of Barrier island stratigraphy and Holocene history of west-central Florida In Davis et. Al (2003), researchers studied the Holocene Barrier island and inner continental shelf located in west-central Florida. The study itself took place in the northern Florida Gulf peninsula barrier inlet, extending from Anclote Key to Cape Romano. The purpose of this research project was to analyze the characteristics and nature of the barriers, as well as to understand where the barriers were formed and the process(s) of that formation.
Kumulipo is a Hawaiian chant that describes the story of creation along with a genealogy of Hawaiian royalty. This story was brought to Hawaii by the marriage of two people, Pi 'ikea and ‘Umi. During the time of the formation of this myth Hawaiia was under the authority of a corrupt monarchy, and the dominant religion on the island was Roman Catholicism. It was first printed in 1889, at the time it was in possession of the ruling king, Kalakaua. The story of creation is told by a series of 16 chants, many containing multiple parts.
I have lived in two distinct communities: the first was the small town of Moraga in the East Bay area of California, the second, and my current residence, is the city of Stockton. The former, Moraga is the epitome of white picket fence suburbia, with friendly neighbors, a high ranking public school system, and a practically non-existent crime rate. Growing up in Moraga, I was able to receive a great education, roam the streets freely with friends, and never had to fear horrors, such as, gang violence, sporadic neighborhood shootings, or drug abuse. Sadly, when I moved to the latter, most of these horrors were apparent weekly, if not daily.
The canyon has colors from the Alabama clay. The rocks are
“Dad check out this lure!” I shouted as I ran towards a big, glittery spoon in the isle of Gander Mountain. The large golden spoon sat on the shelf waiting for a kid like me to come along and fall in love with it. This particular spoon was meant for pike fishing, a bait that twirled around in the water, flashing and catching the attention of a pike.
With the increased scale of fracking in Texas, one might wonder if the oil boom is affecting our water supply. The value of water in Texas is deeply cherished considering Texas’s dry climate and long-standing droughts. One may even wonder if Texas is valuing its water as much as it is its oil. As research furthers, we can begin to weigh the positive and negative effects of oil fracking. By providing overwhelming data on oil fracking
The formation strikes 269°, and dips 41°N. The sandstone and mudstone members are typically 30-50cm thick. The sandstones are immature poorly sorted greywacke, and the mudstones
1. Introduction In 2010, the Deepwater Horizon oil platform spit nearly five million barrels of oil into the Gulf of Mexico, making it the largest oil spill in history. The 1989 oil spill surpassed Exxon Valdez's oil spill in 1989 as the largest oil spill ever seen in US-controlled waters and the Ixtoc I oil spill of 1979 as the largest oil spill in the Gulf of Mexico. On April 20, 2010, Deepwater Horizon, an ultra-deepwater offshore rig, exploded in the Gulf of Mexico about 41 miles off the coast of Louisiana, killing 11 riggers and injuring 17 others.
Since the location was near to the Maribyrnong River, the procedure must be further stimulated by the existence of the river in the ecosystem, and this is happening from the further upstream. As for the downstream, it carried by the sediment that deposited at the riverbanks of the Maribyrnong River. Weathering and erosion of the primary rock in the early stage were leading to the deposition of sediment, and the younger sediment progressively replaced the older sediment which along the riverbank (Figure 2.3). Further away from the Maribyrnong river a little bit where the river flow was gradually rapid, some Marine deposits from the Ordovician Period was found such as mudstone, interbedded shale and greywacke, which may
Exxon exercises unique geoscience capabilities and understanding of the global hydrocarbon endowment to identify and prioritize all quality resources in a cost-effective manner. Exxon’s strategy is a cost leadership strategy in the upstream segment by outperforming the competition—creating a comparable value at low-cost—using core competencies: industry-leading technology and capabilities, disciplined approach to investing and cost management, and operations
The ocean… The sound of the waves applauding and hugging the shore. The internal sounds of the body out in the world’s biggest swimming pool. The echo of my sister’s laughter. The salty smell so strong that one can taste it dancing on ones taste buds.