principal investigator tmc (chandryaan-2) & mcc (mars ... · chandrayaan-1, tmc , orbit 798, 13...
TRANSCRIPT
Principal Investigator –
TMC (Chandryaan-2) &
MCC (Mars Orbiter Mission)
Ch-1 AO Training Prog, SAC, March 2-3, 2017
SARA
11 INSTRUMENTS INBOARD CHANDRYAAN-1
TMC : Terrain Mapping Camera
HySI : Hyper Spectral imager
HEX : High Energy X-ray Spectrometer
LLRI : Lunar Laser Ranging Instrument
MIP : Moon Impact Probe
SARA : SWIM+CENA (Low Energy Neutral Atom + Solar Wind Monitor
CIXS : CH-1 X-ray Spectrometer
MMM (M3) : Moon Mineralogy Mapper
Mini-SAR : Mini - Synth Aperture Radar
RADOM : Radiation Dose Monitor
SIR-2 : Near Infra-Red Spectrometer
0°
TMC NEAR SIDE COVERAGE TMC 90 degree EAST COVERAGE
TMC FAR SIDE COVERAGE TMC 90 degree WEST COVERAGE
90°0°
180°270°
1 5
Direct Observation
Derived Information
2.5 km0
DISSECTED CRATER
HySI Ratio ImageTMC
Fe
Crater Morphology:
Chandrayaan-1, TMC Orbit 798, 13 January, 2009
Location: HERMANN A Crater (Oceanus Procellarum )
Longitude: 58.334 W / Latitude: 0.4 N
~ 3.9 km
Concave failure of the western side of inner wall
HERMANN-A CRATER
Concave Failure
Sharp Rim Edges
3D Perspective View
13.8 km
Damoiseau E Crater
Chandrayaan-1, TMC , Orbit 798, 13 January, 2009, Damoiseau E Crater Longitude: 58.3 E / Latitude: 5.2 S
Slumped Inner slopes
Crater Morphology: Results from TMC
A
B
A B
Cross-Section profile (km)
3
2
1
5 10 15
Slumped Inner slopes
Crater Morphology: Results from TMC
13.8 km
TMC
R-Glassy/Ejecta G/Y – Fe, Illmenite B- Ti BasalticHYSI RATIO FCC
Glassy
Ti
Slumped Inner slopes
Failed Slopes
Floor
Rim
Floor
Failed Slopes
Rim
mts
Relief Slicing
Crater Morphology: Results from TMC
LUNAR STRUCTURES
MORETUS CRATER - TMC
15 November, 2008 (TMC, Nadir)
Probable Fault / Fracture
6.5 km
Lat 70.59S Long 0.09 W,
Plane of Failure
Source: Clementine
movie
886m
LUNAR STRUCTURES
MORETUS CRATER - TMC3D Perspective View
Vertical Drop
Surface Age Determination CSFD
Dome
Cone
DEMContour
Perspective
Slope
CHANDRAYAAN -1 : DOMES & CONES –
A.S. Arya, Guneshwar Thangjam, R.P. Rajasekhar, Ajai, B. Gopala Krishna, Amitabh, A.S. Kiran Kumar, R.R. Navalgund (2011), Morphometric and rheological analysis of an effusive dome in Marius Hills using Chandrayaan-1 TMC Data. 42nd LPSC, Houston, #1470
DomeCone
10.4 km
343m : h
Flank Slope
3.77o
Volume : 8.45 km3
•Morphometry
•Rheology
•Dike Dimensions
•Age Determination
•Surface Composition
45th LPSC 2014, Houston
Catalogue of Lunar Domes (MHR)
CHANDRAYAAN -1 : LATERAL LAVA TUBE : Detection & Dimensional Analysis
A.S. Arya , R P Rajasekhar , Ajai , A.S Kiran Kumar , R..R. Navalgund
Identification Of Lunar Volcanic Tubes, A Potential Site For
Human Settlement Using 3d Chandryaan 1 – Tmc Data,
.
Abs. Proc. 41st LPSC, Houston, 2010 , #1484&
current science Feb 25, 2011
Collapsed
Rille
Collapsed
Rille
Buried Lava Tube
1.9 km
360m
7.36 km
Buried Tube
120m
Arya et. al. , CURRENT SCIENCE, VOL. 102, NO. 5, 10 MARCH 2012
3.69 km
1 28
Arya et al., 2013, Abs Vol., 100th Indian Science Congress, Kolkata
Age Determination of Melt PoolCrater Size Frequency Distribution (CSFD) for a melt pool region showing the age of 34.3 Ma
A lava tube entrance in Hawaii, Rille-bed shows collapse breccia
Lineaments mapped on the central peak (yellow) and the floor (green)
Inner Rim Rose Diagram
Floor Rose Diagram
Central Peak Rose Diagram
Reflectance Anomaly around Apollo-15 Landing site
Aft Nadir Fore
Prakash Chuahan, Ajai & A S Kiran Kumar (2009), Current Science, Vol 97, No. 5,
Coulomb C crater DEM Slope image Slope aspect
cos qs/ cos iTopography corr.
Chandrayaan-1: Photometric Correction
After
Before
1 35
1 36