<s>[INST] You are a smart text analyzer assistant.
Given a QUESTION and a set of posible texts from which to derive the answer, examine each text and reply whether or not the ANSWER exists within the text.
You MUST give the response in a VALID JSON object with a Yes or No for each text.


So for instance the following:

QUESTION: What is the color of the sky?
POSIBLE ANSWERS:
Source 1: The sky is blue
Source 2: The sea is blue
Source 3: The sky is blue in the daytime but black at night

would give an output of:[/INST]

{
"Source 1": "Yes",
"Source 2": "No",
"Source 3": "Yes"
}
</s>
 
[INST]
QUESTION: i-type granite definition
POSIBLE ANSWERS:
Source 1: Granite differs from granodiorite in that at least 35% of the feldspar in granite is alkali feldspar as opposed to plagioclase; it is the potassium feldspar that gives many granites a distinctive pink color. Granites can be predominantly white, pink, or gray in color, depending on their mineralogy. The word granite comes from the Latin granum, a grain, in reference to the coarse-grained structure of such a holocrystalline rock. By definition, granite is an igneous rock with at least 20% quartz and up to 65% alkali feldspar by volume
Source 2: Classification of granites according their magmatic origin results in the formation of two contrasting groups, S-types and I-types. S-types result from the partial melting of metasedimentary source rocks, a process called anatexis or ultrametamorphism. S-type granites com from a source which has been subjected to this sedimentary fractionation. Hine et al (1978) used the Kosciusko Batholith to illustrate chemical differences between S-type and I-type granites. A Na2O/K2O plot of the Kosciusko batholith illustrates the fundamental chemical difference
Source 3: 1 I-type Granites. 2  I-type granites are granites considered to have formed by melting of an original igneous type source. 3  These are generally metaluminous granites, expressed mineralogically by the absence of peraluminous minerals and the absence of peralkaline minerals, as discussed below. A wide variety of igneous rocks occur in the continental lithosphere, a reflection of its heterogeneous nature compared to oceanic lithosphere. In addition, because the continents are not subducted and are subject to uplift and erosion, older plutonic rocks are both preserved and accessible to study.
[/INST]
<s>[INST] You are a smart text analyzer assistant.
Given a QUESTION and a set of posible texts from which to derive the answer, examine each text and reply whether or not the ANSWER exists within the text.
You MUST give the response in a VALID JSON object with a Yes or No for each text.


So for instance the following:

QUESTION: What is the color of the sky?
POSIBLE ANSWERS:
Source 1: The sky is blue
Source 2: The sea is blue
Source 3: The sky is blue in the daytime but black at night

would give an output of:[/INST]

{
"Source 1": "Yes",
"Source 2": "No",
"Source 3": "Yes"
}
</s>
 
[INST]
QUESTION: i-type granite definition
POSIBLE ANSWERS:
Source 1: Granite differs from granodiorite in that at least 35% of the feldspar in granite is alkali feldspar as opposed to plagioclase; it is the potassium feldspar that gives many granites a distinctive pink color. Granites can be predominantly white, pink, or gray in color, depending on their mineralogy. The word granite comes from the Latin granum, a grain, in reference to the coarse-grained structure of such a holocrystalline rock. By definition, granite is an igneous rock with at least 20% quartz and up to 65% alkali feldspar by volume
Source 2: Classification of granites according their magmatic origin results in the formation of two contrasting groups, S-types and I-types. S-types result from the partial melting of metasedimentary source rocks, a process called anatexis or ultrametamorphism. S-type granites com from a source which has been subjected to this sedimentary fractionation. Hine et al (1978) used the Kosciusko Batholith to illustrate chemical differences between S-type and I-type granites. A Na2O/K2O plot of the Kosciusko batholith illustrates the fundamental chemical difference
Source 3: 1 I-type Granites. 2  I-type granites are granites considered to have formed by melting of an original igneous type source. 3  These are generally metaluminous granites, expressed mineralogically by the absence of peraluminous minerals and the absence of peralkaline minerals, as discussed below. A wide variety of igneous rocks occur in the continental lithosphere, a reflection of its heterogeneous nature compared to oceanic lithosphere. In addition, because the continents are not subducted and are subject to uplift and erosion, older plutonic rocks are both preserved and accessible to study.
[/INST]
{
"Source 1": "No",
"Source 2": "Yes",
"Source 3": "Yes"
}
<s>[INST] You are a smart text analyzer assistant.
Given a QUESTION and a set of posible texts from which to derive the answer, examine each text and reply whether or not the ANSWER exists within the text.
You MUST give the response in a VALID JSON object with a Yes or No for each text.


So for instance the following:

QUESTION: What is the color of the sky?
POSIBLE ANSWERS:
Source 1: The sky is blue
Source 2: The sea is blue
Source 3: The sky is blue in the daytime but black at night

would give an output of:[/INST]

{
"Source 1": "Yes",
"Source 2": "No",
"Source 3": "Yes"
}
</s>
 
[INST]
QUESTION: i-type granite definition
POSIBLE ANSWERS:
Source 1: Granite differs from granodiorite in that at least 35% of the feldspar in granite is alkali feldspar as opposed to plagioclase; it is the potassium feldspar that gives many granites a distinctive pink color. Granites can be predominantly white, pink, or gray in color, depending on their mineralogy. The word granite comes from the Latin granum, a grain, in reference to the coarse-grained structure of such a holocrystalline rock. By definition, granite is an igneous rock with at least 20% quartz and up to 65% alkali feldspar by volume
Source 2: Classification of granites according their magmatic origin results in the formation of two contrasting groups, S-types and I-types. S-types result from the partial melting of metasedimentary source rocks, a process called anatexis or ultrametamorphism. S-type granites com from a source which has been subjected to this sedimentary fractionation. Hine et al (1978) used the Kosciusko Batholith to illustrate chemical differences between S-type and I-type granites. A Na2O/K2O plot of the Kosciusko batholith illustrates the fundamental chemical difference
Source 3: 1 I-type Granites. 2  I-type granites are granites considered to have formed by melting of an original igneous type source. 3  These are generally metaluminous granites, expressed mineralogically by the absence of peraluminous minerals and the absence of peralkaline minerals, as discussed below. A wide variety of igneous rocks occur in the continental lithosphere, a reflection of its heterogeneous nature compared to oceanic lithosphere. In addition, because the continents are not subducted and are subject to uplift and erosion, older plutonic rocks are both preserved and accessible to study.
[/INST]
{
"Source 1": "Yes",
"Source 2": "No",
"Source 3": "No"
}