1. Rationale: APPROXIMATE ESTIMATION FOR HYDROTHERMAL BAND: ZONE INSIDE OF EBERSWALDE CRATER Juan C. Echaurren Codelco Chile North Division Fourth MSL.

Slides:



Advertisements
Similar presentations
Putative eroded inverted valley Long/lat: E, 23.93N Rational: Sediments deposited in this filled and inverted valley, at the base of the remnant.
Advertisements

Lobate ejecta from large and fresh crater Long/lat: E, 23.69N E, 23.74N Rational: A crater of diameter ~12 km has exhumed material from.
Contact between layered sulfate & clay bearing strata and fluvial channel at Gale crater Latitude/longitude: 4°46'26" S, 137°23'42" E Rationale: Alteration.
Large craters outside the ellipse Long/lat (by decreasing size): E, 24.24N E, 24.30N E, 24.25N E, 24.32N E,
Phyllosilicate-bearing Trough Latitude/longitude: North, East Rationale: The phyllosilicates exposed here may be lacustrine sediments. Morphology.
1 2 km TARGET INSIDE OF EBERSWALDE CRATER Juan C. Echaurren Codelco Chile North Division Fourth MSL Landing Workshop Latitude/Longitude: °S, °E.
Large fractures (to be differentiated from the small polygonal fracturation) Long/lat: (no particular order) E, 23.84N E, 23.85N E,
Breccia at Mawrth: polygonal breccia & breccia in elongate pods Latitude/longitude: 1) 24° 8'40"N, 18°53'55"W 2) 24° 8'55"N, 18°53'40"W Rationale: Interesting.
Reflection Field Methods
Mound-Skirting Unit Outcrop and Inverted Channel Latitude/longitude: North, East Rationale: This outcrop may be an alluvial fan or part of.
Remnant buttes Long/lat: (in random order) E, 23.89N E, 23.95N E, 23.98N E, 24.04N E, 24.05N E, 24.14N.
Ancient eroded layered craters Long/lat : (ranked by distance from ellipse center) E, 24.05N E, 24.01N E, 23.98N E, 23.86N.
Light-toned sulfate/clay layer at Gale crater Latitude/longitude: X North, Y East Rationale: Location of transition between phyllosilicate-rich units and.
Crater Floor Stratigraphy Latitude/longitude: North, East Rationale: Several crater floor units are exposed in close proximity to each other.
Erosion-resistant Polygonal Ridges Latitude/longitude: North, East Rationale: These features are widespread in Gale crater and may be cemented.
Phyllosilicate-bearing outcrop within the Eberswalde Crater landing ellipse Latitude/longitude: North, East Rationale: This brecciated,
Large valleys north of landing site Long/lat: from E, 24.26N to E, 24.58N Rational: Sediments deposited in these valleys may be of utmost interest.
Lowest Strata in Gale Mound (near landing site) Latitude/longitude: 4°47'30"S, 137°17'50”E Rationale: Base of the exposed stratigraphic section for the.
Lower blue unit Long/lat: E, 23.97N Rational: This different mineralogy reveals different conditions of formation/alteration. Morphology & mineralogy:
Contact between putative delta and brecciated substrate in western Eberswalde Crater Latitude/longitude: North, East Rationale: Phyllosilicate-bearing,
Eroded Crater at Mawrth: at least 2 generations of fill. Latitude/longitude: 24° 2'20"N, 18°56'20"W (previously proposed but with different rationale)
Lower blue unit Long/lat: E, 23.97N Rational: This different mineralogy reveals different conditions of formation/alteration, maybe due to hydrothermal.
Embedded Crater at Mawrth: possible crater within stratigraphy in the wall of a younger crater Latitude/longitude: 23°26'55"N, 18°52'20"W Rationale: Provides.
1 Simplifying the martian carbon dioxide cycle: An empirical method for predicting surface pressure Paul Withers 1, Silvia Tellmann Boston University.
Light-Toned Ridge Latitude/longitude: North, East Rationale: A prominent part of the stratigraphy of the Gale mound, containing phyllosilicates.
EXAMPLE 3 Use areas to find a geometric probability The diameter of the target shown at the right is 80 centimeters. The diameter of the red circle on.
Project Idea Fire potential models can help stratify and reduce the number of false positive fire ‘detections’ by assigning probability levels to the landscape.
Coastal Zones The Coastal Region.
Earthquakes BY-Ahmed Ali 707 Ms.Azcona.
Clipping: Clipping is a process of dividing an object into visible and invisible positions and displaying the visible portion and discarding the invisible.
NASA’s Live Simulations Featuring: Target Moon. Scenario The Comet Named KC2035. Newly discovered. Might impact the moon as close as 1,500 km from one.
PRELIMINARY ANALYSIS; FOR DISCUSSION PURPOSES ONLY File name: MSLOutcomes_v11.ppt Potential MSL Outcomes and Discovery Response Joy Crisp, David Beaty,
MSL Status/Update for MEPAG John Grotzinger 1, Joy Crisp 2, and Ashwin Vasavada 2 1 California Institute of Technology 2 Jet Propulsion Laboratory, California.
Impact Crater Lakes and the Astrobiological Exploration of Mars NASA Astrobiology Institute Mars Focus Group Videocon (01/08/01) Nathalie A. Cabrol NASA.
赴国际水稻所访学情况汇报 长江大学农学院 邢丹英 2010 年 6 月. 学习目的 学习时间、地点 学习内容 学习收获 几点体会 汇报提纲.
Course 2 Image Filtering. Image filtering is often required prior any other vision processes to remove image noise, overcome image corruption and change.
Life in the Atacama Life in the Atacama 2004 Science & Technology Workshop July 14-16, 2004 Carnegie Mellon University.
Finding your way in the world. Latitude lines are imaginary lines that run EAST/WEST (horizontally) around the earth's surface. Think of latitude like.
Measurability – MSL payload instruments Based on definitive nature of the biosignature and its measurability by the MSL payload o diagnostic organic molecules.
The Third Moscow Solar System Symposium 8 – 12 October 2012, Moscow, Russia First Data from DAN Instrument onboard MSL Curiosity Rover M. Litvak and I.
MSL Science Team Field Site Discussions — Eberswalde CraterEdgett, p. 1 Eberswalde Crater MSL Candidate Field Site in Context by K. Edgett, 9 June 2010.
Software used: ArcMap , MatLab R2015b, Google Earth 7.1.5
CfE Advanced Higher Physics
Dawn Interaction of Energy and Matter: Dawn Mission Instrumentation Framing Cameras 1.
Determining surface characteristics at candidate MSL landing sites using THEMIS high-resolution orbital thermal inertia data Robin Fergason Philip Christensen.
Enabling Capabilities A Robotic Field Geologist Access to a site mapped from orbit Long life, mobility, capability to explore a local region Remote sensing.
Search for Life on MARS. Q: Why is water important for life? A: Because it’s such a great solute.
Cassini-Hugyens Mission Image Gallery. Cassini-Hugyens Mission Image Gallery The Cassini- Huygens spacecraft launched from Cape Canaveral Air Station.
Mars Science Laboratory 1st Landing Site Workshop Pasadena, CA — 31 May – 2 June Fine-layered Meridiani crater for the MSL Landing Site L. V. Posiolova,
11.5 Areas of Circles and Sectors Unit IIIH Day 5.
Interpretations of Fractions. Part of a whole In this interpretation we take a whole object and ‘split it’ into equal parts. Two equal parts are called.
Gale Crater Stratigraphic Measurements and Preliminary Interpretations Ryan Anderson April, 2009.
Here is a picture of a Geoboard. You can make shapes on the board by wrapping a rubber band around the nails.
南水北调东线第一期工程山东段 情况简介. 主要汇报内容 二、南水北调山东段工程总体布置 三、山东段工程项目划分及工程主 要建设内容 一、南水北调东线工程概况 四、前期工作及工程建设进展情况 五、工程总投资.
网上报账系统包括以下业务: 日常报销 差旅费报销 借款业务 1. 填写报销内容 2. 选择支付方式 (或冲销借款) 3. 提交预约单 4. 打印预约单并同分类粘 贴好的发票一起送至财务 处 预约报销步骤: 网上报账系统 薪酬发放管理系统 财务查询系统 1.
Good morning! August 8, Good morning! August 8, 2017.
Seismic network of landers on Mars: Proposed positioning of landing ellipses and evaluation of the encountered range of slopes Michael G., Hauber E., Oberst,
Application of network flow: Protecting coral reef ecosystems
MODEL WIND FIELD COMPARE WITH HRD WIND FIELD
Impact Crater Lakes and the Astrobiological Exploration of Mars
5 million ha of north-west Namibia
The Microscope.
Soil Moisture Active Passive (SMAP) Satellite
Going to Gale Crater Matt Golombek Mars Exploration Program Landing Site Scientist, JPL Malin and Edgett 2000.
My friend measured and said this beam is below where the extra studs need to be placed in the room above. That wire coming out is the wire from the outlet.
Ашық сабақ 7 сынып Файлдар мен қапшықтар Сабақтың тақырыбы:
Windows басқару элементтері
Қош келдіңіздер!.
Информатика пән мұғалімі : Аитова Карима.
Presentation transcript:

1. Rationale: APPROXIMATE ESTIMATION FOR HYDROTHERMAL BAND: ZONE INSIDE OF EBERSWALDE CRATER Juan C. Echaurren Codelco Chile North Division Fourth MSL Landing Workshop Latitude/Longitude/Window of Probability 1: ~  S,  E ; 2: ~  S,  E Is shown here, the hydrothermal band that was predicted with the models used, and the intersection between this band, and one portion of the “Delta”. This intersection defines a window of probability, which, generates the possibility of finding traces of microscopic life on that region. The edges of this window are not absolute, i.e., targets can be located around of them, and targets can be located around of the hydrothermal band too. 2. Morphology and Mineralogy: Possibility of to find argillaceous limestone, and traces of microscopic organic life. 3. What will the rover specifically do here? The rover will use the CheMin instrument for to detect traces of argillaceous limestone.

2.8 km 2 1 Intersection between, a portion of the hydrothermal band, and a portion of the “Delta” (window of probability) Hydrothermal band of ~ km

2.88 km Intersection between, a portion of the hydrothermal band, and a portion of the “Delta” (window of probability) m 2 1 Window of Probability