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Aparaca Construções Sociedade Unipessoal Lda,
K.Venkat Reddy

 Licence No : 7767 L



 Area (Ha) : 7861.36 ,
 DISTRICT : BARUE,
 PROVINCE : MANICA,
 COUNTRY : MOZAMBIQUE



Location Plan
 INTRODUTION:
 Location: 7767 L Mine is located near to Nhampassa Village, Barue District, Manica Province, Mozambique.
 Access : well connected access to Mine is from Guro and Catandica is near to Nhampassa Village, Barue District,
Manica Province, Mozambique.
 Drainage of Area: All area is well connected drendtic pattern of drainage with small rivers and tributaries. Most of
the water flows towards W→E,SE direction .
 Regoinal Geology of the area: This area is belongs to Proterozoic period of age of rocks, south gondwana basin
minerals of Barue complex.
 Báruè Complex –The bulk of Proterozoic rocks along the eastern margin of the
 Zimbabwe Craton, south of the Mungári latitude to almost the Save River, is attributedto theBáruè Complex. Typical
lithologies comprise quartzose, feldspathicand micaceous gneisses and migmatites with minor intercalations of
quartzite,marble and mafic rocks in places. The sedimentary protoliths of these lithologiescorrespond most likely to
monotonous turbidite sequences deposited on the passive
 margin of the Zimbabwe Craton.
 Barue Complex divided in to :
 Chimoio Group – Quartzo-feldspathic and micaceous gneisses and migmatites
 and siliciclastic metasediments.
 Macossa Group – Comprises substantial quantities of amphibole-bearing
 gneisses, hornblendite, calc-silicate rock and marble. The lowermost rock units of the inferred palaeobasin include
garnetiferous leucocratic
 gneisses, quartz-feldspar gneisses, meta-arkoses and arkosic quartzites. These psammitic metasediments are
overlain by more pelitic rocks (metagreywackes, garnet and sillimanite bearing mica schist and mica gneisses) with
thin calc-silicate gneiss .
 The Guro suite comprising Foliated aplitic granite ,Migmaties alternating with meta gabbros, mafic migmatitic roks.
 Lithology : The Báruè Complex is composed of a variety of medium- to high-grade gneisses, migmatites
 and granitoids, with subordinate intercalations of mafic rocks, quartzites, marbles and
 associated calc-silicate rocks.
 The Mine 7767L area is comprise of various metamorphic rocks such as Mica schist, Micaeous Gneisses, pegmatite
dykes, pegmatite Gneisses, ferruginous quartzites, quartzo feldspathic gneisses etc.
 This area also consists of Sedimentary rocks like ferruginous laterites, lateriti red soils on the surface,
 The pegmatites are associated with micaeous gneisses, schists, Gneisses having strike direction N-S dipping 90° .
these Pegmatites consist of Gem variety of Tourmaline,Rubelite,aquamarine,morganite in the area. Gneisses are
covered most of the area consist of micaeous ,pegmatite’s, quartzite’s etc.
 Muscovite, biotite, flogophyte variety of mica found in the area.
 Micaeous gneisses are stikeing N-S , diping 90° towards E-W trending. These are comprises gem baring pegmatite
dykes in the area.
Current working Area 7767L Aparaca Mining Lda.
Weathered Gneiss with Pegmatite Dyke strike N-S, Dip→W 75°,36 K 526517,
8043223
Gneiss with Pegmatite dykes with Tourmaline, 36 K 526536,
8043262
Weathered Gneiss with Pegmatite dyke strike N-S, Dip 40°→W
Major lineations, 36 K 526287, 8043179
Weathered Pegmatite with
Tourmaline crystals,
Micaceous Gniess with Pegmatite dyke, strikes N-S, 36
K 521270, 8045059
Weathered Pegmatite ,Quarz with Tourmmalline Crystals,
At 36 K 526562, 8043284.
Weathered Pegmatite dyke,36K 521227,8045105
Pit - Pegmatite with Muscowhite Mica strike N-S , 36 K
521543, 8037786.
Pegmatite with Mica,Tourmalline Crystals.
APARAA 7767L NHAMPASSA MINE

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APARAA 7767L NHAMPASSA MINE

  • 1. Aparaca Construções Sociedade Unipessoal Lda, K.Venkat Reddy
  • 2.   Licence No : 7767 L     Area (Ha) : 7861.36 ,  DISTRICT : BARUE,  PROVINCE : MANICA,  COUNTRY : MOZAMBIQUE   
  • 4.
  • 5.
  • 6.
  • 7.
  • 8.
  • 9.
  • 10.
  • 11.
  • 12.
  • 13.
  • 14.
  • 15.
  • 16.
  • 17.  INTRODUTION:  Location: 7767 L Mine is located near to Nhampassa Village, Barue District, Manica Province, Mozambique.  Access : well connected access to Mine is from Guro and Catandica is near to Nhampassa Village, Barue District, Manica Province, Mozambique.  Drainage of Area: All area is well connected drendtic pattern of drainage with small rivers and tributaries. Most of the water flows towards W→E,SE direction .  Regoinal Geology of the area: This area is belongs to Proterozoic period of age of rocks, south gondwana basin minerals of Barue complex.  Báruè Complex –The bulk of Proterozoic rocks along the eastern margin of the  Zimbabwe Craton, south of the Mungári latitude to almost the Save River, is attributedto theBáruè Complex. Typical lithologies comprise quartzose, feldspathicand micaceous gneisses and migmatites with minor intercalations of quartzite,marble and mafic rocks in places. The sedimentary protoliths of these lithologiescorrespond most likely to monotonous turbidite sequences deposited on the passive  margin of the Zimbabwe Craton.  Barue Complex divided in to :  Chimoio Group – Quartzo-feldspathic and micaceous gneisses and migmatites  and siliciclastic metasediments.  Macossa Group – Comprises substantial quantities of amphibole-bearing  gneisses, hornblendite, calc-silicate rock and marble. The lowermost rock units of the inferred palaeobasin include garnetiferous leucocratic  gneisses, quartz-feldspar gneisses, meta-arkoses and arkosic quartzites. These psammitic metasediments are overlain by more pelitic rocks (metagreywackes, garnet and sillimanite bearing mica schist and mica gneisses) with thin calc-silicate gneiss .  The Guro suite comprising Foliated aplitic granite ,Migmaties alternating with meta gabbros, mafic migmatitic roks.  Lithology : The Báruè Complex is composed of a variety of medium- to high-grade gneisses, migmatites  and granitoids, with subordinate intercalations of mafic rocks, quartzites, marbles and  associated calc-silicate rocks.  The Mine 7767L area is comprise of various metamorphic rocks such as Mica schist, Micaeous Gneisses, pegmatite dykes, pegmatite Gneisses, ferruginous quartzites, quartzo feldspathic gneisses etc.  This area also consists of Sedimentary rocks like ferruginous laterites, lateriti red soils on the surface,  The pegmatites are associated with micaeous gneisses, schists, Gneisses having strike direction N-S dipping 90° . these Pegmatites consist of Gem variety of Tourmaline,Rubelite,aquamarine,morganite in the area. Gneisses are covered most of the area consist of micaeous ,pegmatite’s, quartzite’s etc.  Muscovite, biotite, flogophyte variety of mica found in the area.  Micaeous gneisses are stikeing N-S , diping 90° towards E-W trending. These are comprises gem baring pegmatite dykes in the area.
  • 18. Current working Area 7767L Aparaca Mining Lda.
  • 19.
  • 20.
  • 21.
  • 22. Weathered Gneiss with Pegmatite Dyke strike N-S, Dip→W 75°,36 K 526517, 8043223
  • 23. Gneiss with Pegmatite dykes with Tourmaline, 36 K 526536, 8043262
  • 24. Weathered Gneiss with Pegmatite dyke strike N-S, Dip 40°→W Major lineations, 36 K 526287, 8043179
  • 26. Micaceous Gniess with Pegmatite dyke, strikes N-S, 36 K 521270, 8045059
  • 27. Weathered Pegmatite ,Quarz with Tourmmalline Crystals, At 36 K 526562, 8043284.
  • 29. Pit - Pegmatite with Muscowhite Mica strike N-S , 36 K 521543, 8037786.