Degree of bioturbation.ppt
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The document discusses sediment samples that show: 1) Intensely bioturbated mudstone with a high diversity of burrows including Phycosiphon, Teichichnus, Planolites, Chondrites, and Rhizocorallium. 2) Cross-bedded sediments with clay draped foresets, bidirectional flow, and thick bottomsets that are flaser bedded with variable bioturbation and burrows including Planolites, Macaronichnus, Ophiomorpha, and Thalassinoides, indicating a tidal channel environment. 3) Bioturbated mudstone and laminated mudstone that is sparsely or intensely bioturbated with
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Degree of bioturbation.ppt
The document describes observations from sedimentology studies including descriptions of lithology, sedimentary structures, degree of bioturbation, ichnofauna diversity, and burrow organization. Specific observations noted include muddy heterolithic sediments that were intensely bioturbated with high diversity including traces of Phycosiphon, Teichichnus, Planolites, and Chondrites indicative of an inner shelf environment. Definitions of bioturbation and bioerosion are also provided from previous literature.
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This is a ppt that was used in my confirmation for candidature. It describes how I will use stable isotope and fatty acid analysis to determine what estuarine sharks and rays eat and which areas of the South Alligator River, (NT, Aus) they utilise. This will then inform environmental managers of which areas are critical to the survival of these species.
Lesson 1 The Ecosystem.pptx
The document provides an overview of ecosystems, including definitions, components, and classifications. It defines an ecosystem as a system where biotic and abiotic factors interact. It describes trophic structures and food chains, with producers, primary consumers, secondary consumers, and decomposers. It also discusses gradients, ecotones, and the importance of diversity at the genetic, species, and ecosystem levels. Ecosystems are classified as either natural or artificial, with natural ecosystems further divided into aquatic (marine and freshwater) and terrestrial systems. Examples of different ecosystem types are provided.
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How does differ from evolution systematic Only cladistics traces e.pdf
How does differ from evolution systematic Only cladistics traces e.pdf
PhD confirmation - ecology of estuarine sharks & rays
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leaves.ppt
The document describes several landforms produced by wave erosion along coastlines, including headlands, bays, wave-cut notches, wave-cut platforms, arches, caves, stacks, and blowholes. Headlands are areas that jut out into the sea, often ending in cliffs, while bays are wide curved inlets. Wave action can erode cliffs from below, forming platforms, notches, arches that eventually collapse into stacks and stumps. Blowholes form through joints in cliff rocks exposed to hydraulic action inside wave-eroded caves.
Formation of headlands and bays.ppt
Waves eroding a coastline of varying rock resistance will form headlands of harder rock separated by bays in weaker rock. Landforms produced by wave erosion include headlands, bays, stacks, caves, arches, pillars, and wave-cut platforms and notches. Caves can develop into blowholes if joints in the rock connect the cave to the cliff top.
bedding planes.ppt
The document describes several landforms produced by wave erosion along coastlines including:
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- Headlands, which are parts of the coastline that jut out into the sea, often ending in cliffs.
- Bays, which are wide curved inlets formed along coastlines with weaker, more erodible rock.
- Arches and caves, which are openings formed when waves erode through headlands or into cliffs.
leaves a stump..ppt
Waves erode cliffs and headlands through various processes, forming different coastal landforms. Caves form where waves attack both sides of headlands. Arches may form if caves erode all the way through. Stacks and stumps are left when arches and stacks eventually collapse. Over time, this differential erosion of harder and weaker rocks creates a series of alternating headlands and bays along the coastline.
Formation of headlands and bays.ppt
This document describes several landforms produced by wave erosion along coastlines:
- Headlands jut out into the sea at the end of cliffs. Bays form sheltered inlets in weaker coastal rocks between headlands.
- Arches form when waves erode caves completely through headlands. Stacks are isolated pillars that remain when arches collapse.
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Formation of headlands and bays.ppt
The document describes various landforms produced by wave erosion along coastlines including headlands, bays, wave-cut notches, wave-cut platforms, arches, caves, stacks, and blowholes. It explains how waves erode harder and softer rocks at different rates, forming headlands in harder rocks and sheltered bays in weaker rocks. Arches form when waves erode caves through headlands, and stacks remain when arches collapse, eventually becoming stumps.
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Stratigraphic principles and sequence stratigraphy are methods used to analyze sedimentary rock layers and impose a temporal dimension. Key concepts include:
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Submarine canyons cut across continental shelves and slopes, carrying sediment from rivers and coastal areas to deep ocean basins. Submarine fans form at the mouths of canyons, accumulating sediment across the continental slope in a fan-shaped pattern. Sediment transport within submarine fans occurs through various mechanisms like debris flows, density currents, and turbidity currents, resulting in deposition of turbidite sequences that can be studied to understand ancient submarine fan environments.
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This document summarizes a study of the Floridan Aquifer/Chipola River System funded by the USGS and FDEP. The objectives are to identify nutrient sources to the aquifer, characterize hydrologic transport processes using modeling, and match nitrate concentrations in springs using the model. The study area includes the Dougherty Karst Plain where the Floridan Aquifer is recharged through sinkholes and rivers. A MODFLOW model is being used to simulate nitrate tracking from recharge areas and calibrate to spring discharge concentrations. Local grid refinement is being added to improve flow path and travel time estimates in key springs.
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Sediments form through the weathering and erosion of rocks, followed by transportation and deposition. There are three main types of sediments: mechanical (clastic), chemical, and organic. Sedimentary rocks form through the compaction and cementation of sediments via the process of diagenesis. Sedimentology involves the study of sediment formation and depositional environments, while stratigraphy examines the temporal and spatial relationships between sedimentary strata. Key methods used in sedimentology include facies analysis, particle size and shape analysis, lithological analysis, and stratigraphic mapping and description.
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The document discusses various methods used to prevent sloughing during well drilling operations. Specifically:
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2. Circulating brine through the well below the freezing point of water to freeze the formation.
3. Circulating mud-laden fluid through the well below the freezing point of water to freeze the formation.
4. Circulating an emulsion through the well below the freezing point of water to freeze the formation.
5. Causing fluid to flow into the well to seep into the formation, then circulating it below the freezing point of water to freeze the formation
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The document discusses methods for drilling wells through formations containing sloughing shale to prevent borehole collapse.
It describes 6 methods:
1. Circulating refrigerated fluid through the well to freeze the formation, with the refrigerant having a freezing point below that of the formation fluid.
2. Circulating brine through the well and cooling it to freeze the formation, with the brine's freezing point below that of water.
3. Circulating mud-laden fluid through the well in the same way as method 2.
4. Circulating an emulsion through the well in the same way as methods 2 and 3.
5. Causing fluid to flow into the well to contact
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The document discusses the problem of sloughing shale during drilling operations. Sloughing shale occurs when the mud weight is not adequate to control subsurface pressure or the mud salinity causes undesirable osmotic pressure, leading to borehole collapse and stuck drill pipes or bottom hole assembly (BHA). It states that sloughing shale is one of the mechanical issues that can cause stuck pipes. The author provides a personal anecdote about experiencing BHA getting stuck in sloughing shale for the first time and seeing large cuttings, which was shocking. While shale formations can be drilled quickly when conditions are right, sloughing shale turns it into a stressful problem similar to kicks, losses, and other drilling hazards. Close
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一比一原版(USF毕业证)旧金山大学毕业证如何办理
原件一模一样【微信：95270640】【旧金山大学毕业证USF学位证成绩单】【微信：95270640】（留信学历认证永久存档查询）采用学校原版纸张、特殊工艺完全按照原版一比一制作（包括：隐形水印，阴影底纹，钢印LOGO烫金烫银，LOGO烫金烫银复合重叠，文字图案浮雕，激光镭射，紫外荧光，温感，复印防伪）行业标杆！精益求精，诚心合作，真诚制作！多年品质 ,按需精细制作，24小时接单,全套进口原装设备，十五年致力于帮助留学生解决难题，业务范围有加拿大、英国、澳洲、韩国、美国、新加坡，新西兰等学历材料，包您满意。
【业务选择办理准则】
一、工作未确定，回国需先给父母、亲戚朋友看下文凭的情况，办理一份就读学校的毕业证【微信：95270640】文凭即可
二、回国进私企、外企、自己做生意的情况，这些单位是不查询毕业证真伪的，而且国内没有渠道去查询国外文凭的真假，也不需要提供真实教育部认证。鉴于此，办理一份毕业证【微信：95270640】即可
三、进国企，银行，事业单位，考公务员等等，这些单位是必需要提供真实教育部认证的，办理教育部认证所需资料众多且烦琐，所有材料您都必须提供原件，我们凭借丰富的经验，快捷的绿色通道帮您快速整合材料，让您少走弯路。
留信网认证的作用:
1:该专业认证可证明留学生真实身份【微信：95270640】
2:同时对留学生所学专业登记给予评定
3:国家专业人才认证中心颁发入库证书
4:这个认证书并且可以归档倒地方
5:凡事获得留信网入网的信息将会逐步更新到个人身份内，将在公安局网内查询个人身份证信息后，同步读取人才网入库信息
6:个人职称评审加20分
7:个人信誉贷款加10分
8:在国家人才网主办的国家网络招聘大会中纳入资料，供国家高端企业选择人才
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我们所定的价格是非常合理的，而且我们现在做得单子大多数都是代理和回头客户介绍的所以一般现在有新的单子 我给客户的都是第一手的代理价格，因为我想坦诚对待大家 不想跟大家在价格方面浪费时间
对于老客户或者被老客户介绍过来的朋友，我们都会适当给一些优惠。
选择实体注册公司办理，更放心，更安全！我们的承诺：可来公司面谈，可签订合同，会陪同客户一起到教育部认证窗口递交认证材料，客户在教育部官方认证查询网站查询到认证通过结果后付款，不成功不收费！
办理旧金山大学毕业证毕业证学位证USF学位证【微信：95270640 】外观非常精致，由特殊纸质材料制成，上面印有校徽、校名、毕业生姓名、专业等信息。
办理旧金山大学毕业证USF学位证毕业证学位证【微信：95270640 】格式相对统一，各专业都有相应的模板。通常包括以下部分：
校徽：象征着学校的荣誉和传承。
校名:学校英文全称
授予学位：本部分将注明获得的具体学位名称。
毕业生姓名：这是最重要的信息之一，标志着该证书是由特定人员获得的。
颁发日期：这是毕业正式生效的时间，也代表着毕业生学业的结束。
其他信息：根据不同的专业和学位，可能会有一些特定的信息或章节。
办理旧金山大学毕业证毕业证学位证USF学位证【微信：95270640 】价值很高，需要妥善保管。一般来说，应放置在安全、干燥、防潮的地方，避免长时间暴露在阳光下。如需使用，最好使用复印件而不是原件，以免丢失。
综上所述，办理旧金山大学毕业证毕业证学位证USF学位证【微信：95270640 】是证明身份和学历的高价值文件。外观简单庄重，格式统一，包括重要的个人信息和发布日期。对持有人来说，妥善保管是非常重要的。
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一比一原版(uoft毕业证书)加拿大多伦多大学毕业证如何办理
原版一模一样【微信：741003700 】【(uoft毕业证书)加拿大多伦多大学毕业证成绩单】【微信：741003700 】学位证，留信认证（真实可查，永久存档）原件一模一样纸张工艺/offer、雅思、外壳等材料/诚信可靠,可直接看成品样本，帮您解决无法毕业带来的各种难题！外壳，原版制作，诚信可靠，可直接看成品样本。行业标杆！精益求精，诚心合作，真诚制作！多年品质 ,按需精细制作，24小时接单,全套进口原装设备。十五年致力于帮助留学生解决难题，包您满意。
本公司拥有海外各大学样板无数，能完美还原。
1:1完美还原海外各大学毕业材料上的工艺：水印，阴影底纹，钢印LOGO烫金烫银，LOGO烫金烫银复合重叠。文字图案浮雕、激光镭射、紫外荧光、温感、复印防伪等防伪工艺。材料咨询办理、认证咨询办理请加学历顾问Q/微741003700
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三.真实教育部学历学位认证（教育部存档！教育部留服网站永久可查）
四.办理各国各大学文凭(一对一专业服务,可全程监控跟踪进度)
如果您处于以下几种情况：
◇在校期间，因各种原因未能顺利毕业……拿不到官方毕业证【q/微741003700】
◇面对父母的压力，希望尽快拿到；
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◇回国时间很长，忘记办理；
◇回国马上就要找工作，办给用人单位看；
◇企事业单位必须要求办理的
◇需要报考公务员、购买免税车、落转户口
◇申请留学生创业基金
留信网认证的作用:
1:该专业认证可证明留学生真实身份
2:同时对留学生所学专业登记给予评定
3:国家专业人才认证中心颁发入库证书
4:这个认证书并且可以归档倒地方
5:凡事获得留信网入网的信息将会逐步更新到个人身份内，将在公安局网内查询个人身份证信息后，同步读取人才网入库信息
6:个人职称评审加20分
7:个人信誉贷款加10分
8:在国家人才网主办的国家网络招聘大会中纳入资料，供国家高端企业选择人才
办理(uoft毕业证书)加拿大多伦多大学毕业证【微信：741003700 】外观非常简单，由纸质材料制成，上面印有校徽、校名、毕业生姓名、专业等信息。
办理(uoft毕业证书)加拿大多伦多大学毕业证【微信：741003700 】格式相对统一，各专业都有相应的模板。通常包括以下部分：
校徽：象征着学校的荣誉和传承。
校名:学校英文全称
授予学位：本部分将注明获得的具体学位名称。
毕业生姓名：这是最重要的信息之一，标志着该证书是由特定人员获得的。
颁发日期：这是毕业正式生效的时间，也代表着毕业生学业的结束。
其他信息：根据不同的专业和学位，可能会有一些特定的信息或章节。
办理(uoft毕业证书)加拿大多伦多大学毕业证【微信：741003700 】价值很高，需要妥善保管。一般来说，应放置在安全、干燥、防潮的地方，避免长时间暴露在阳光下。如需使用，最好使用复印件而不是原件，以免丢失。
综上所述，办理(uoft毕业证书)加拿大多伦多大学毕业证【微信：741003700 】是证明身份和学历的高价值文件。外观简单庄重，格式统一，包括重要的个人信息和发布日期。对持有人来说，妥善保管是非常重要的。
FUNDAMENTALS OF MECHANICAL ENGINEERING.pdf
EMERSON EDUARDO RODRIGUES
EMERSON EDUARDO RODRIGUES
EMERSON EDUARDO RODRIGUES
EMERSON EDUARDO RODRIGUES
EMERSON EDUARDO RODRIGUES
EMERSON EDUARDO RODRIGUES
EMERSON EDUARDO RODRIGUES
EMERSON EDUARDO RODRIGUES
EMERSON EDUARDO RODRIGUES
EMERSON EDUARDO RODRIGUES
EMERSON EDUARDO RODRIGUES
原版制作(Humboldt毕业证书)柏林大学毕业证学位证一模一样
原件一模一样【微信：bwp0011】《(Humboldt毕业证书)柏林大学毕业证学位证》【微信：bwp0011】学位证，留信认证（真实可查，永久存档）原件一模一样纸张工艺/offer、雅思、外壳等材料/诚信可靠,可直接看成品样本，帮您解决无法毕业带来的各种难题！外壳，原版制作，诚信可靠，可直接看成品样本。行业标杆！精益求精，诚心合作，真诚制作！多年品质 ,按需精细制作，24小时接单,全套进口原装设备。十五年致力于帮助留学生解决难题，包您满意。
本公司拥有海外各大学样板无数，能完美还原。
1:1完美还原海外各大学毕业材料上的工艺：水印，阴影底纹，钢印LOGO烫金烫银，LOGO烫金烫银复合重叠。文字图案浮雕、激光镭射、紫外荧光、温感、复印防伪等防伪工艺。材料咨询办理、认证咨询办理请加学历顾问微bwp0011
【主营项目】
一.毕业证【微bwp0011】成绩单、使馆认证、教育部认证、雅思托福成绩单、学生卡等！
二.真实使馆公证(即留学回国人员证明,不成功不收费)
三.真实教育部学历学位认证（教育部存档！教育部留服网站永久可查）
四.办理各国各大学文凭(一对一专业服务,可全程监控跟踪进度)
如果您处于以下几种情况：
◇在校期间，因各种原因未能顺利毕业……拿不到官方毕业证【微bwp0011】
◇面对父母的压力，希望尽快拿到；
◇不清楚认证流程以及材料该如何准备；
◇回国时间很长，忘记办理；
◇回国马上就要找工作，办给用人单位看；
◇企事业单位必须要求办理的
◇需要报考公务员、购买免税车、落转户口
◇申请留学生创业基金
留信网认证的作用:
1:该专业认证可证明留学生真实身份
2:同时对留学生所学专业登记给予评定
3:国家专业人才认证中心颁发入库证书
4:这个认证书并且可以归档倒地方
5:凡事获得留信网入网的信息将会逐步更新到个人身份内，将在公安局网内查询个人身份证信息后，同步读取人才网入库信息
6:个人职称评审加20分
7:个人信誉贷款加10分
8:在国家人才网主办的国家网络招聘大会中纳入资料，供国家高端企业选择人才
Blood finder application project report (1).pdf
Blood Finder is an emergency time app where a user can search for the blood banks as
well as the registered blood donors around Mumbai. This application also provide an
opportunity for the user of this application to become a registered donor for this user have
to enroll for the donor request from the application itself. If the admin wish to make user
a registered donor, with some of the formalities with the organization it can be done.
Specialization of this application is that the user will not have to register on sign-in for
searching the blood banks and blood donors it can be just done by installing the
application to the mobile.
The purpose of making this application is to save the user’s time for searching blood of
needed blood group during the time of the emergency.
This is an android application developed in Java and XML with the connectivity of
SQLite database. This application will provide most of basic functionality required for an
emergency time application. All the details of Blood banks and Blood donors are stored
in the database i.e. SQLite.
This application allowed the user to get all the information regarding blood banks and
blood donors such as Name, Number, Address, Blood Group, rather than searching it on
the different websites and wasting the precious time. This application is effective and
user friendly.
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