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EXPLORING ON MARS - THE RED PLANET

ARUNSENAPATHY R
11/6/2013

1
PRESENTATION OUTLINE
 OBJECTIVES
 MARS | AT A GLANCE
 IMPACT CRATERS ON MARS
 REASON FOR OCCURRENCE
 BIGGEST CRATERS ON MARS

 MARS MISSIONS
 PLANETARY ROVING VEHICLES ON MARS | HISTORY & COMPARISON
 CONCLUSION

 REFERENCE

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OBJECTIVES
 TO UNDERSTAND THE ESSENTIALS OF MARS

 TO KNOW ABOUT IMPACT CRATERS ON MARS AND THE REASON FOR

OCCURRENCE

 TO DISCUSS ABOUT THE BIGGEST IMPACT CRATERS ON MARS

 TO COGNIZE THE MODERN INNOVATIONS IN MARS

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MARS | AT A GLANCE

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MARS


FOURTH PLANET FROM THE SUN | SECOND SMALLEST
PLANET IN THE SOLAR SYSTEM



NAMED AFTER THE ROMAN GOD OF WAR



DESCRIBED AS THE “RED PLANET”



THE IRON OXIDE PREVALENT ON ITS SURFACE GIVES IT A
REDDISH APPEARANCE


11/6/2013

A TERRESTRIAL PLANET WITH A THIN ATMOSPHERE
5
MARS - THE RED PLANET



MARS SURFACE IS COMPRISED OF IRONRICH MINERALS (RUST OR OXIDIZE) AND
DUST.

 THE MARTIAN SURFACE IS NOT ALL RUST-COLORED, HOWEVER,
BECAUSE DEPENDING ON THE OXIDATION PROCESS, THE MINERALS
CAN BE A RANGE OF COLORS FROM BUTTERSCOTCH TO RUST.
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MARS LOCATION

MARS

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MARS FACTS
 DISTANCE FROM SUN ≈1.52 TIMES AS FAR AS EARTH
 TIME TO ORBIT THE SUN ~ 26 EARTH MONTHS
 ATMOSPHERE ~ MOSTLY CARBON DIOXIDE
 MARTIAN DAY ~ 24.7 HOURS
 TEMPERATURE ON THE PLANET’S SURFACE HARDLY RISES ABOVE

FREEZING POINT

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8
EARTH AND MARS | COMPARISON
PARTICULARS

EARTH

MARS

RADIUS

6378 KM

3397 KM

DENSITY

5515 KG/M3

3933 KG/M3

GRAVITY

9.8 M/S2

3.72 M/S2

YEAR

365.25 DAYS

686.98 DAYS

ECCENTRICITY

0.017

0.094

DAY

24 HOURS

24 HR 39 MIN

OBLIQUITY

23.45º

25.19º

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9
CONTD…

THE LAND AREA OF EARTH IS APPROXIMATELY EQUAL TO THE
TOTAL SURFACE OF MARS

THE LAND AREA OF AFRICA IS ABOUT THE SAME
AS THE TOTAL SURFACE OF THE MOON

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MARS | SURFACE FEATURES


SURFACE COLOR “RED”



FEATURES
 IMPACT CRATERS
 LARGEST VOLCANO IN THE SOLAR
SYSTEM
(OLYMPUS MONS)
 LARGEST CANYON IN THE SOLAR

SYSTEM
(VALLES MARINERIS)
 ANCIENT RIVER CHANNELS

VALLES MARINERIS

 LAVA ROCKS
 DUST: REDDISH FROM VOLCANIC
ROCK

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MARS | ATMOSPHERE
 UNBREATHABLE
 THIN
 DUSTY, MAKES THE SKY PINKISH, LOTS
OF DUST STORMS
 SURFACE PRESSURE: 1/150TH OF EARTH’S

(ONLY 5.6 MILLIBARS)
 COMPOSITION: 95% CO2, 3% N, 1.5% AR,
0.1% O2, 0.03% H2O

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MOONS OF MARS

PHOBOS

 MARS HAS TWO TINY MOONS NAMED “DEIMOS” (PANIC) & “PHOBOS” (FEAR)

Deimos

 THE MOONS ARE IRREGULAR AND VERY SMALL IN SIZE
 PHOBOS 27X22X18 KM
 DEIMOS 15X12X10 KM
 THE MOONS ARE PROBABLY ASTEROIDS CAPTURED BY MARS

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WATER ON MARS
 WATER IS THE KEY TO LIFE AS WE KNOW IT
 THE NORTH AND SOUTH POLES OF MARS ARE COVERED WITH THICK ICE
OR FROST
 SOME ASTRONOMERS ABOUT 100 YEARS AGO THOUGHT THERE WERE
CANALS ON MARS DUG BY INTELLIGENT CIVILIZATION

 SPACE PROBES TO DATE HAVE NOT FOUND ANY TRACES OF CANALS ON
MARS

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IMPACT CRATERS ON MARS

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 IMPACT CRATER IN MARS IS A LARGE HOLE IN THE GROUND CAUSED BY A

METEORITE SMASHING INTO THE SURFACE OF MARS
 EVERY SOLID BODY IN THE SOLAR SYSTEM SUFFERS FROM THE EFFECTS OF
IMPACT CRATERING
 THE PROJECTILES THAT CAUSE IMPACT CRATERS, TRAVEL AT VERY HIGH SPEED

AND FASTER

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TERMINOLOGIES
 CENTRAL PEAK - A MOUNTAIN FORMED IN THE CENTRE OF LARGE IMPACT
CRATERS. THESE DO NOT OCCUR IN SMALL IMPACT CRATERS
 EJECTA - A SHEET OF MATERIAL (ROCKS, SOIL) SURROUNDING THE CRATER
THAT WAS THROWN OUT DURING THE IMPACT EVENT
 ERODE - THE PROCESS BY WHICH SOMETHING IS WORN AWAY OVER TIME
 FLOOR - THE FLOOR OF AN IMPACT CRATER (USUALLY EITHER FLAT OR BOWLSHAPED), LYING BELOW THE SURROUNDING GROUND LEVEL
 IMPACT CRATER - A HOLE IN THE GROUND (USUALLY CIRCULAR) CAUSED BY
THE IMPACT OF A METEORITE ONTO THE SURFACE OF A SOLID BODY

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CONTD…

 METEORITE - A LUMP OF ROCK OR ICE THAT HITS THE SURFACE OF A
PLANETARY BODY

 PROJECTILE - AN OBJECT THAT STRIKES A SURFACE TO PRODUCE AN IMPACT
CRATER. THESE CAN INCLUDE DUST PARTICLES, PEBBLES, ROCKS, COMETS
AND ASTEROIDS
 RAISED RIM - THIS IS THE EDGE OF THE IMPACT CRATER AND IS COMPOSED OF

ROCKS AND MATERIAL PILED UP ON TOP OF ONE ANOTHER
 RAYS - BRIGHT LINES OF EJECTA COMING FROM AN IMPACT CRATER. THESE
CAN EXTEND FOR VAST DISTANCES IN THE CASE OF LARGE IMPACTS
 TERRACED WALLS - THESE ONLY OCCUR IN LARGE IMPACT CRATERS. AFTER

THE CRATER FORMS, THE WALLS OF THE CRATER SLIP, CREATING HUGE
LANDSLIDES INSIDE THE CRATER

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REASON FOR OCCURRENCE OF IMPACT
CRATERS ON MARS

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 FORMED BY A LARGE OBJECT SUCH AS AN ASTEROID OR A COMET
 WHEN THESE LARGE OBJECTS HIT THE SURFACE THEY FORM HOLES (CRATERS)
 LATE HEAVY BOMBARDMENT PERIOD OF OUR SOLAR SYSTEM
 NO ATMOSPHERE TO PROTECT IT FROM ASTEROIDS

 THAT'S WHY MARS HAS CRATERS

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PHOTOGRAPHS OF VARIOUS IMPACT CRATERS
ON MARS

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CONTD…

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BIGGEST CRATERS ON MARS

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BOREALIS BASIN
 8,500 – KM IN DIAMETER
 A HUGE 4 BILLION YEAR-OLD IMPACT CRATER

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25
CONTD…

HELLAS BASIN
 OVER 2,100 KILOMETERS IN DIAMETER AND NINE KILOMETERS DEEP
 THE HELLAS BASIN ON THE SOUTHERN HEMISPHERE OF MARS IS VERY
BIG, AND VERY DEEP

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CONTD…

ARGYRE BASIN
 SECOND TO HELLAS IN TERMS OF SIZE.
 THE MASSIVE ARGYRE BASIN ON THE SOUTHERN HEMISPHERE OF MARS.
 1,800 KILOMETRES



WIDE AND 5 KM IN DIAMETER

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MARS MISSIONS

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NASA - MARS SCIENCE LABORATORY [MSL]
CURIOSITY ROVER

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PHOTOGRAPHS OF CURIOSITY ROVER

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CONTD…

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31
CONTD…

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32
PLANETARY ROVING VEHICLES ON MARS
HISTORY & COMPARISON

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MARINER - MARS
(MARINER-4 TOGETHER WITH MARINER-3)

 OPERATOR NASA
 MISSION TYPE FLYBY
 LAUNCH DATE NOVEMBER 28, 1964

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SPIRIT ROVER

 OPERATOR NASA

 MISSION TYPE ROVER
 LAUNCH DATE JUNE 10, 2003

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OPPORTUNITY ROVER

 OPERATOR NASA

 MISSION TYPE ROVER
 LAUNCH DATE JULY 07, 2003

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PHOENIX
 OPERATOR NASA
 MISSION TYPE LANDER
 LAUNCH DATE MAY 25, 2008

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CURIOSITY

 OPERATOR NASA

 MISSION TYPE ROVER
 LAUNCH DATE NOVEMBER 26, 2011

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COMPARISON OF PLANETARY ROVING
VEHICLES ON MARS

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39
CONTD…

11/6/2013

40
MARS ORBITER MISSION
MARS ORBITER MISSION IS INDIA'S FIRST INTERPLANETARY MISSION TO
PLANET MARS WITH AN ORBITER CRAFT DESIGNED TO ORBIT MARS IN AN
ELLIPTICAL ORBIT.
THE MISSION IS PRIMARILY TECHNOLOGICAL MISSION CONSIDERING THE
CRITICAL MISSION OPERATIONS AND STRINGENT REQUIREMENTS ON
PROPULSION AND OTHER BUS SYSTEMS OF SPACECRAFT.
SUCCESSFULLLY LAUNCHED ON 5 NOVEMBER 2013, 09:08 UTC IN PSLV-XL
C25 ROCKET FROM SATISH DHAWAN SPACE CENTRE (SDSC)

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MARS ORBITER MISSION – LAUNCH IMAGES

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42
CONCLUSION

 A BASIC OUTLINE TO IMPACT CRATERS IS DISCUSSED

 IMPACT CRATERS ON MARS AND THE REASON FOR OCCURRENCE WERE
DELIBERATED

 MODERN INNOVATIONS IN MARS WERE CONFERRED

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43
REFERENCES
[1] T. BARATA, E. I. ALVES, J. SARAIVA, AND P. PINA, “AUTOMATIC RECOGNITION OF
IMPACT CRATERS ON THE SURFACE OF MARS,” IMAGE ANALYSIS AND

RECOGNITION, VOL. 3212, LECTURE NOTES IN COMPUTER SCIENCE. NEWYORK:
PRINGER-VERLAG, 2004, PP. 489–496.

[2] “TEN BIGGEST IMPACT CRATERS IN THE SOLAR SYSTEM” BY “SCIENCE PHOTO
LIBRARY FEATURE STORIES”

[3] TEANBY, N.A., WOOKEY, J., SEISMIC DETECTION OF METEORITE IMPACTS ON
MARS, PHYSICS OF THE EARTH AND PLANETARY INTERIORS (2010), DOI:10.1016 /
J.PEPI.2011.03.004
[4] http://www.isro.org/pslv-c25/mission.aspx
11/6/2013

44
THANK YOU

CONTACT DETAILS

ARUNSENAPATHY R | PROJECT ASSOCIATE
PLANETARY SCIENCES AND EXPLORATION PROGRAMME | PLANEX DIVISION
PHYSICAL RESEARCH LABORATORY | A UNIT OF DEPT. OF SPACE, GOVT. OF INDIA
NAVRANGPURA | AHMEDABAD | 380 009 | INDIA | www.prl.res.in
MOBILE +91-9558549700 | E-MAIL senaarun@prl.res.in (OFFICIAL) | senaarun@gmail.com (PERSONAL)

11/6/2013

45

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EXPLORING ON MARS - THE RED PLANET

  • 1. EXPLORING ON MARS - THE RED PLANET ARUNSENAPATHY R 11/6/2013 1
  • 2. PRESENTATION OUTLINE  OBJECTIVES  MARS | AT A GLANCE  IMPACT CRATERS ON MARS  REASON FOR OCCURRENCE  BIGGEST CRATERS ON MARS  MARS MISSIONS  PLANETARY ROVING VEHICLES ON MARS | HISTORY & COMPARISON  CONCLUSION  REFERENCE 11/6/2013 2
  • 3. OBJECTIVES  TO UNDERSTAND THE ESSENTIALS OF MARS  TO KNOW ABOUT IMPACT CRATERS ON MARS AND THE REASON FOR OCCURRENCE  TO DISCUSS ABOUT THE BIGGEST IMPACT CRATERS ON MARS  TO COGNIZE THE MODERN INNOVATIONS IN MARS 11/6/2013 3
  • 4. MARS | AT A GLANCE 11/6/2013 4
  • 5. MARS  FOURTH PLANET FROM THE SUN | SECOND SMALLEST PLANET IN THE SOLAR SYSTEM  NAMED AFTER THE ROMAN GOD OF WAR  DESCRIBED AS THE “RED PLANET”  THE IRON OXIDE PREVALENT ON ITS SURFACE GIVES IT A REDDISH APPEARANCE  11/6/2013 A TERRESTRIAL PLANET WITH A THIN ATMOSPHERE 5
  • 6. MARS - THE RED PLANET  MARS SURFACE IS COMPRISED OF IRONRICH MINERALS (RUST OR OXIDIZE) AND DUST.  THE MARTIAN SURFACE IS NOT ALL RUST-COLORED, HOWEVER, BECAUSE DEPENDING ON THE OXIDATION PROCESS, THE MINERALS CAN BE A RANGE OF COLORS FROM BUTTERSCOTCH TO RUST. 11/6/2013 6
  • 8. MARS FACTS  DISTANCE FROM SUN ≈1.52 TIMES AS FAR AS EARTH  TIME TO ORBIT THE SUN ~ 26 EARTH MONTHS  ATMOSPHERE ~ MOSTLY CARBON DIOXIDE  MARTIAN DAY ~ 24.7 HOURS  TEMPERATURE ON THE PLANET’S SURFACE HARDLY RISES ABOVE FREEZING POINT 11/6/2013 8
  • 9. EARTH AND MARS | COMPARISON PARTICULARS EARTH MARS RADIUS 6378 KM 3397 KM DENSITY 5515 KG/M3 3933 KG/M3 GRAVITY 9.8 M/S2 3.72 M/S2 YEAR 365.25 DAYS 686.98 DAYS ECCENTRICITY 0.017 0.094 DAY 24 HOURS 24 HR 39 MIN OBLIQUITY 23.45º 25.19º 11/6/2013 9
  • 10. CONTD… THE LAND AREA OF EARTH IS APPROXIMATELY EQUAL TO THE TOTAL SURFACE OF MARS THE LAND AREA OF AFRICA IS ABOUT THE SAME AS THE TOTAL SURFACE OF THE MOON 11/6/2013 10
  • 11. MARS | SURFACE FEATURES  SURFACE COLOR “RED”  FEATURES  IMPACT CRATERS  LARGEST VOLCANO IN THE SOLAR SYSTEM (OLYMPUS MONS)  LARGEST CANYON IN THE SOLAR SYSTEM (VALLES MARINERIS)  ANCIENT RIVER CHANNELS VALLES MARINERIS  LAVA ROCKS  DUST: REDDISH FROM VOLCANIC ROCK 11/6/2013 11
  • 12. MARS | ATMOSPHERE  UNBREATHABLE  THIN  DUSTY, MAKES THE SKY PINKISH, LOTS OF DUST STORMS  SURFACE PRESSURE: 1/150TH OF EARTH’S (ONLY 5.6 MILLIBARS)  COMPOSITION: 95% CO2, 3% N, 1.5% AR, 0.1% O2, 0.03% H2O 11/6/2013 12
  • 13. MOONS OF MARS PHOBOS  MARS HAS TWO TINY MOONS NAMED “DEIMOS” (PANIC) & “PHOBOS” (FEAR) Deimos  THE MOONS ARE IRREGULAR AND VERY SMALL IN SIZE  PHOBOS 27X22X18 KM  DEIMOS 15X12X10 KM  THE MOONS ARE PROBABLY ASTEROIDS CAPTURED BY MARS 11/6/2013 13
  • 14. WATER ON MARS  WATER IS THE KEY TO LIFE AS WE KNOW IT  THE NORTH AND SOUTH POLES OF MARS ARE COVERED WITH THICK ICE OR FROST  SOME ASTRONOMERS ABOUT 100 YEARS AGO THOUGHT THERE WERE CANALS ON MARS DUG BY INTELLIGENT CIVILIZATION  SPACE PROBES TO DATE HAVE NOT FOUND ANY TRACES OF CANALS ON MARS 11/6/2013 14
  • 15. IMPACT CRATERS ON MARS 11/6/2013 15
  • 16.  IMPACT CRATER IN MARS IS A LARGE HOLE IN THE GROUND CAUSED BY A METEORITE SMASHING INTO THE SURFACE OF MARS  EVERY SOLID BODY IN THE SOLAR SYSTEM SUFFERS FROM THE EFFECTS OF IMPACT CRATERING  THE PROJECTILES THAT CAUSE IMPACT CRATERS, TRAVEL AT VERY HIGH SPEED AND FASTER 11/6/2013 16
  • 18. TERMINOLOGIES  CENTRAL PEAK - A MOUNTAIN FORMED IN THE CENTRE OF LARGE IMPACT CRATERS. THESE DO NOT OCCUR IN SMALL IMPACT CRATERS  EJECTA - A SHEET OF MATERIAL (ROCKS, SOIL) SURROUNDING THE CRATER THAT WAS THROWN OUT DURING THE IMPACT EVENT  ERODE - THE PROCESS BY WHICH SOMETHING IS WORN AWAY OVER TIME  FLOOR - THE FLOOR OF AN IMPACT CRATER (USUALLY EITHER FLAT OR BOWLSHAPED), LYING BELOW THE SURROUNDING GROUND LEVEL  IMPACT CRATER - A HOLE IN THE GROUND (USUALLY CIRCULAR) CAUSED BY THE IMPACT OF A METEORITE ONTO THE SURFACE OF A SOLID BODY 11/6/2013 18
  • 19. CONTD…  METEORITE - A LUMP OF ROCK OR ICE THAT HITS THE SURFACE OF A PLANETARY BODY  PROJECTILE - AN OBJECT THAT STRIKES A SURFACE TO PRODUCE AN IMPACT CRATER. THESE CAN INCLUDE DUST PARTICLES, PEBBLES, ROCKS, COMETS AND ASTEROIDS  RAISED RIM - THIS IS THE EDGE OF THE IMPACT CRATER AND IS COMPOSED OF ROCKS AND MATERIAL PILED UP ON TOP OF ONE ANOTHER  RAYS - BRIGHT LINES OF EJECTA COMING FROM AN IMPACT CRATER. THESE CAN EXTEND FOR VAST DISTANCES IN THE CASE OF LARGE IMPACTS  TERRACED WALLS - THESE ONLY OCCUR IN LARGE IMPACT CRATERS. AFTER THE CRATER FORMS, THE WALLS OF THE CRATER SLIP, CREATING HUGE LANDSLIDES INSIDE THE CRATER 11/6/2013 19
  • 20. REASON FOR OCCURRENCE OF IMPACT CRATERS ON MARS 11/6/2013 20
  • 21.  FORMED BY A LARGE OBJECT SUCH AS AN ASTEROID OR A COMET  WHEN THESE LARGE OBJECTS HIT THE SURFACE THEY FORM HOLES (CRATERS)  LATE HEAVY BOMBARDMENT PERIOD OF OUR SOLAR SYSTEM  NO ATMOSPHERE TO PROTECT IT FROM ASTEROIDS  THAT'S WHY MARS HAS CRATERS 11/6/2013 21
  • 22. PHOTOGRAPHS OF VARIOUS IMPACT CRATERS ON MARS 11/6/2013 22
  • 24. BIGGEST CRATERS ON MARS 11/6/2013 24
  • 25. BOREALIS BASIN  8,500 – KM IN DIAMETER  A HUGE 4 BILLION YEAR-OLD IMPACT CRATER 11/6/2013 25
  • 26. CONTD… HELLAS BASIN  OVER 2,100 KILOMETERS IN DIAMETER AND NINE KILOMETERS DEEP  THE HELLAS BASIN ON THE SOUTHERN HEMISPHERE OF MARS IS VERY BIG, AND VERY DEEP 11/6/2013 26
  • 27. CONTD… ARGYRE BASIN  SECOND TO HELLAS IN TERMS OF SIZE.  THE MASSIVE ARGYRE BASIN ON THE SOUTHERN HEMISPHERE OF MARS.  1,800 KILOMETRES  WIDE AND 5 KM IN DIAMETER 11/6/2013 27
  • 29. NASA - MARS SCIENCE LABORATORY [MSL] CURIOSITY ROVER 11/6/2013 29
  • 30. PHOTOGRAPHS OF CURIOSITY ROVER 11/6/2013 30
  • 33. PLANETARY ROVING VEHICLES ON MARS HISTORY & COMPARISON 11/6/2013 33
  • 34. MARINER - MARS (MARINER-4 TOGETHER WITH MARINER-3)  OPERATOR NASA  MISSION TYPE FLYBY  LAUNCH DATE NOVEMBER 28, 1964 11/6/2013 34
  • 35. SPIRIT ROVER  OPERATOR NASA  MISSION TYPE ROVER  LAUNCH DATE JUNE 10, 2003 11/6/2013 35
  • 36. OPPORTUNITY ROVER  OPERATOR NASA  MISSION TYPE ROVER  LAUNCH DATE JULY 07, 2003 11/6/2013 36
  • 37. PHOENIX  OPERATOR NASA  MISSION TYPE LANDER  LAUNCH DATE MAY 25, 2008 11/6/2013 37
  • 38. CURIOSITY  OPERATOR NASA  MISSION TYPE ROVER  LAUNCH DATE NOVEMBER 26, 2011 11/6/2013 38
  • 39. COMPARISON OF PLANETARY ROVING VEHICLES ON MARS 11/6/2013 39
  • 41. MARS ORBITER MISSION MARS ORBITER MISSION IS INDIA'S FIRST INTERPLANETARY MISSION TO PLANET MARS WITH AN ORBITER CRAFT DESIGNED TO ORBIT MARS IN AN ELLIPTICAL ORBIT. THE MISSION IS PRIMARILY TECHNOLOGICAL MISSION CONSIDERING THE CRITICAL MISSION OPERATIONS AND STRINGENT REQUIREMENTS ON PROPULSION AND OTHER BUS SYSTEMS OF SPACECRAFT. SUCCESSFULLLY LAUNCHED ON 5 NOVEMBER 2013, 09:08 UTC IN PSLV-XL C25 ROCKET FROM SATISH DHAWAN SPACE CENTRE (SDSC) 11/6/2013 41
  • 42. MARS ORBITER MISSION – LAUNCH IMAGES 11/6/2013 42
  • 43. CONCLUSION  A BASIC OUTLINE TO IMPACT CRATERS IS DISCUSSED  IMPACT CRATERS ON MARS AND THE REASON FOR OCCURRENCE WERE DELIBERATED  MODERN INNOVATIONS IN MARS WERE CONFERRED 11/6/2013 43
  • 44. REFERENCES [1] T. BARATA, E. I. ALVES, J. SARAIVA, AND P. PINA, “AUTOMATIC RECOGNITION OF IMPACT CRATERS ON THE SURFACE OF MARS,” IMAGE ANALYSIS AND RECOGNITION, VOL. 3212, LECTURE NOTES IN COMPUTER SCIENCE. NEWYORK: PRINGER-VERLAG, 2004, PP. 489–496. [2] “TEN BIGGEST IMPACT CRATERS IN THE SOLAR SYSTEM” BY “SCIENCE PHOTO LIBRARY FEATURE STORIES” [3] TEANBY, N.A., WOOKEY, J., SEISMIC DETECTION OF METEORITE IMPACTS ON MARS, PHYSICS OF THE EARTH AND PLANETARY INTERIORS (2010), DOI:10.1016 / J.PEPI.2011.03.004 [4] http://www.isro.org/pslv-c25/mission.aspx 11/6/2013 44
  • 45. THANK YOU CONTACT DETAILS ARUNSENAPATHY R | PROJECT ASSOCIATE PLANETARY SCIENCES AND EXPLORATION PROGRAMME | PLANEX DIVISION PHYSICAL RESEARCH LABORATORY | A UNIT OF DEPT. OF SPACE, GOVT. OF INDIA NAVRANGPURA | AHMEDABAD | 380 009 | INDIA | www.prl.res.in MOBILE +91-9558549700 | E-MAIL senaarun@prl.res.in (OFFICIAL) | senaarun@gmail.com (PERSONAL) 11/6/2013 45